Book. Jbte // 1887 Resources of Dakota. Ad Official Publication Compiled by the COMMISSIONER OF IMMIGRATION, Under Authority Granted by the Territcrial Legislature. CONTAINING DESCRIPTIVE STATEMENTS AND GENERAL INFORMATION RE- LATING TO THE SOIL, CLIMATE, PRODUCTIONS; ADVANTAGES AND DEVELOPMENT— AGRICULTURAL, MANUFACTURING, COM- MERCIAL, AND MINERAL— THE GEOGRAPHY AND TOPOGRAPHY OF THE TERRITORY. The Vacant Public Lands AND HOW TO OBTAIN THEM; TOGETHER WITH DIAGRAMS, STATEMENTS, TABLES AND SUMMARIES SHOWING THE PRODUCTS AND PROGRESS OF THE TERRITORY AND OF EACH COUNTY, SEPARATELY. TERRITORY OF DAKOTA! DEPARTMENT OF IMMIGRATION AND STATISTICS. P. F. McCLURE, COMMISSIONER, PIERRE. SIOUX FALLS, DAKOTA : ARGUS-LEADER COMPANY, PRINTEBS. 1887. ^•5 % oo oo o M * o Eh O g g s sa p 2 p p p 5 P-" CO oo, ,ooooooo©o©oooOo , r i © - o o o u- o in o o o o o o ~P eNCir-TfNCNCNf o OOgo O O O © < r-^CN £££ CD CD <5 CQ ;P £ O oj d W ^ S S &q : i -1 ■ ' G o3 ** : -«t3 3 * a) OEt 5?S '„ W ^ K- ■ i- ,S ■< a> ir m -«3 vg £ (B O W ffl 5o^s ^ c "T ft'S ;H)B.O-3 P0Q^£ S< §« ©«< ^-o 5 •CD . . o> >! t7 " m ^g^§°|2 8ft Sg,,. bd O co ~ >> — - a ^ x -o j -G c tTT! ^ o g o> > g'C> P§S a>.2 i. " 1% £ g • _ .2S5j^ r Q ! =~cS^«.S^ < »eSX5 0J 2 5 5 ° i S-a©t^c3d?© O CD K^^« P ^ x fe II •h 03 ;©---- * £ : - : B o .2 s Z = 5 >s- < z !S E -1 K X - 8" X ■a; s Ph - i ^ ~ Si oj Oj o 33 p. ed tn 3 3 cc = = o ki - 1 — < y< "2 2 = ^ o - j5 OJ o j^PhhSSS^-WW 1 2 w <

3 o' s ^On-AHpqQ g p ^i «d 06 ail o< 2 r-o> (« t. » Ol O 0) £ceH m £ «S o <0 Sh a) Ci ACKNOWLEDGMENTS. Credit is due A. T. Andreas, compiler of Andreas' Historical Atlas of Dakota ; Dr. T. C. Duncan, editor of the United States Medical Investiga- tor, Chicago, and publisher of several pamphlets descriptive of Dakota ; Kand, McNally & Co., Chicago, publishers of the Bankers' Directory; O. H. Holt, compiler of ''Dakota, 1885;" and to the newspapers generally throughout the Territory for much of the data contained in this work. Thanks are also returned to the county auditors, clerks and treasurers ; city clerks and postmasters; ministers, colleges, organizations and individ- uals, on whom (owing to the lack of any efficient law governing the collec- tion and compilation of the statistics of the Territory), the compher^has depended for favors and assistance in obtaining local information. INTRODUCTORY.— DAKOTA IN 1887. THE PROGRESS AND DEVELOPMENT OF THE TERRITORY DURING THE PAST YEAR. The Territory has had another year of wonderful growth in population and wealth. The reports from all sections tell of a decided increase of im- migration as compared with the same date of last year, and that the rush of newcomers has kept well up to the average of previous seasons. As a mat- ter of course the localities along the line of the railway extensions, and the districts having large areas of the public domain subject to entry under the homestead and pre-emption laws, are receiving the greatest number of settlers. Generally speaking, the people who go West to find homes are those of limited means, either having met with reverses or else just making a start in life, and are attracted to a new country by the cheapness of the lands. Therefore it is quite to be expected, so long as there remains land to be had for the asking, with just as rich soil, just as nutritious pasturage as that of the older settled regions, the larger per cent, of the home-seek- ers will flow into those counties where the whistle of the locomotive is never heard or where the sound is a reverberation from the distance. Then, too, Dakota's past development assures the newcomer that, no matter how great the extent of virgin soil surrounding him to-day, to- morrow he will be on the confines of a thrifty village, with schools, churches, and a busy, bustling, Western town at his very door. The Right Rev. William H. Hare, missionary bishop of southern Dakota, writing to the New York Herald, tells in graphic words of the rapid growth of new communities in the Territory. The bishop says: " Language cannot exaggerate the rapidity with which these communi- ties are built up. You ["may stand ankle deep in the short burnt grass of an uninhabited wilderness — next month a mixed train will glide over the waste and stop at some point where the railway has decided to locate a town. Men, women and children will jump out of the cars, and their chat- tels will be tumbled out after them. From that moment the building be- gins. The courage and faith of these pioneers are something extraordi- nary. Their spirit seems to rise above all obstacles. I have ridden into a Dakota valley and pitched my tent. After my supper, lolling upon my buffalo robe, I have looked around and seen nothing but a wolf that looked 8 RESOURCES OF DAKOTA. down from a hill into the valley to see who the intruder was. When I vis- ited that valley the next year, I saw a long train of Pullman palace cars. In that same trip I camped on the flat bottom land near the Missouri river. There was no sign of civilization there but a log hut with a mud roof. It was the home of a Frenchman who had married an Indian woman. With- in the year I revisited the spot and saw a town. It has increased since to 2,000." The county of this year, the name of which is learned only by consult- ing the map, may next harvest contribute to the world's food-supply a mil- lion bushels of wheat of the finest grade known to the markets of the globe. IMMIGRATION. The building westward through the northern counties of Dakota of the St. Paul, Minneapolis and Manitoba railroad, and the construction by this and the Northern Pacific railway companies of numerous north and south feeders have turned a great tide of immigration toward the splendid agri- cultural and stock lands of the Mouse river, Turtle Mountains, Devils Lake and other regions thereby made easily accessible. This, together with the largest crop ever harvested in many sections of northern Dakota, has made it almost impossible to keep pace with the development going on in the districts named. A few of the more westerly counties, having scarcely a single inhabitant at the beginning of the year, are now well populated with thrifty farmers and residents of the towns which have grown up literally in a day. The increased activity in the line of railway building through the central portion of the Territory, and the fine crops gathered by the farmers there, together with a considerable quantity of land remaining vacant in many of the counties adjacent to the Missouri river, have attracted a large number of people to these localities. Early in the spring a large colony of settlers, coming direct from Ver- mont and New England points, located in Hettinger county, about twenty- five miles south of the Northern Pacific railway. Although this colony decided upon a location in an unsurveyed and almost unexplored county, nevertheless its members have already established a town, erected com- fortable homes and harvested an abundant crop. Their successful venture insures for the future a heavy immigration to the large area of vacant lands of the west Missouri country — especially from the New England and Mid- dle states. The Red River valley in the north and all the counties of older Dakota in the south, central and east, with their large number of growing and prosperous cities, have long since reached that stage of stability, wealth and independence which insures a constant and ever-increasing ratio of added population and improvement. Here the splendidly developed forms and busy towns, full of enterprise, rivalry and life, give one the im- pression of living in a state of many years' growth, rather than in a Terri- tory of youthful age. RESOURCES OF DAKOTA. 9 The completion last year of a line of railway to Rapid City and the cer- tainty of the addition, at an early date, of other railway facilities, has re- sulted in a marked growth of the varied interests of the Black Hills coun- try by placing that hitherto isolated section in better communication with theEastern world. Nature has certainly lavished her gifts upon that area of Dakota, known as the Black Hills, with a generous hand, and it but re- mains for man to enact his small part in order to develop here the richest, grandest region in all the Union. What with the productive soil of her valleys and foothills, the splendid pasturage and excellent protection fur- nished her herds of cattle, sheep and other stock, and her inex- haustible supply of precious minerals, iron, tin, mica, salt, coal, gyp- sum, asbestos, petroleum and other valuable deposits, the saying that the Black Hills might be walled in by an impassable barrier and still be self- supporting, is almost a truism. During the year ending June 30, 1887, 2,007, 281 acres of the public do- main in Dakota were newly filed on, and our population at that time, based on careful estimates, having the business transacted by the several United States land offices in the Territory as a foundation, amounted to very nearly 570,000. As Dakota's immigration this year averages about 7,000 new- comers each month, it is easy to see that we shall have, by the end of December, 1887, a population of quite 000,000. In addition to the annual rush of seekers after free land, there have been, throughout the Territory — especially in those sections where the supply of Government land is pretty well exhausted — an unusual number of pur- chasers of cheap deeded lands. In many of the counties having railroads, school houses, flourishing towns and the other advantages of old settled communities, deeded land is to be had at a small advance over what it cost the original settler for improvements and Government fees. Owing to the rapid advance in the market value of Dakota realty, these opportunities of obtaining good deeded lands at so low a price, cannot last a great while longer, and discreet investors will accept them wherever offered. The agricultural, manufacturing, commercial and mining interests are all receiving their share of the wealth of investment that has been pouring into the Territory for several years past, and the outlook generally may be considered a very happy one. CROPS OF THE YEAR. And now that the season is ended, the farmers of every locality, be it north, central or south Dakota, the Black Hills or the Red River valley, all are more than gratified with Nature's kind return of a bountiful harvest. The farmer's vocation, as well as other callings, is not always attended with success, and the glorious hopes of spring and summer ofttimes end only in a disappointment of the expected harvest. And especially has this been true of the year 1887 in many localities of the West and Northwest, where the most disastrous failures known for years are the sole record of a sum- mer's labor and toil on the part of the farmer. 10 RESOURCES' OF. DAKOTA. Dakota, however, adds another to her annual records of marvelous har- vests, and conies before the world with the grandest yield ever credited to any state of the Union. The snows of the winter placed the ground in ex- cellent shape for spring work; plowing, seeding, harrowing, and the various farming operations followed from the first of March with little or no interruption from bad weather; April showers vivified and nourished the germ and the warm summer days of May and June strengthened and matured its growth, and July and August saw the weather propitious for har- vesting and the final operations of saving and housing the crop. It now remains but to state that the thresher has proved the truth of our asser- tions made earlier in the season, viz.: that Dakota's wheat crop harvested in 1887 not -only exceeds any previous record of this grand Territory, and the record of any state of the Union, but will amount to one-seventh the entire crop of the United States in 1886. As for corn, no one in the years past could have even harbored a hope that the Territory would ever be able to herald forth a yield in any one season exceeding 20,000,000 bushels of that crop. But such is a fact, and with the probability, too, of increasing that amount considerably if the splendid condition and mag- nificent showing of this crop continue to the close of the % harvest season. Barley, oats, rye, flax, buckwheat and vegetables never promised better, and taking the average throughout the length and breadth of the Terri- tory, Dakota, in all her wonderful career, never produced the equal of the crops of 1887. There may be localities where the lack of moisture at the proper time or other until vorable circumstances, has resulted in unsatisfactory returns to the farmer ; but, when we consider the vast surface of the Territory, equaling in extent the combined area of all of New England, together with the states of New York and Pennsylvania, it can never be expected d season will be so generally favorable as to result in a perfect crop to every county. There has been comparatively little damage from hail or other disastrous storms, and no loss whatever from ravages by chinch bugs. For the whole Territory the yield of the crops for 1887 is far above the average of any previous season, and this occurring in a year of quite general misfortune to farmers elsewhere, is certain to insure to Dakota an era of greater pro- gress, wider fame and heavier immigration than ever before. THE GROWTH OP DAKOTA CITIES AND TOWNS. The growth of Dakota towns is simply marvelous. The oldest resident, one who has long been accustomed to the push and activity of western life, can scarcely keep pace with the changes at present occurring about him. Electric lights, water works, street railways, artesian wells, graded streets, and public improvements of every description, are being added to the list of advantages heralded forth by such of the older cities as had not already accomplished these feats of enterprise. RESOURCES OF DAKOTA. U RAILROAD EXTENSIONS. As for railway extensions, those already completed and others projected and under contract, they puzzle the most careful map-maker in his at- tempt to outline them all. A Dakota town old enough to be divested of swaddling clothes, and without expectations of additional railway facili- ties, is yet to be heard of. Though -the season for railway building is not 3^et passed, more than seven hundred miles of completed track have been added to the 3,491 to the credit of the Territory on the first of January, 1887, making the railroad mileage of Dakota to-day 4,207 miles, and lines are being still further extended in all directions. The four great railway corporations of the Northwest, viz.: the Chicago, Milwaukee and St. Paul, the Chicago and Northwestern, the Northern Pa- cific, and the St. Paul, Minneapolis and Manitoba, are extending their main and branch lines wherever there remains a tempting morsel of un- occupied territory. Then, too, a spirit of rivalry and competition in the matter of obtaining a share in the traffic of prosperous localities, has sprung up between the railway corporations named which can only end to the great advantage of the farmers and shippers of the Territory in cheapening the cost of transportation. The Northern Pacific has completed a line covering the rich Valley of the Red River, from Grand Forks to Pembina, (through counties hitherto traversed only by the St. Paul, Minneapolis and Manitoba), and has ex- tended its Fargo and Southwestern branch from La Moure to Edgely, connecting there with the Chicago, Milwaukee and St. Paul, and furnish- ing a new line of communication between the systems north and south. The St. Paul, Minneapolis and Manitoba, not content with the accom- plishment of the most stupendous feat of railway construction on record — building, since the first of April, 1887, some five hundred miles of track between Minot, Ward county, Dakota, and Great Falls, Montana, at the rate of from five to ten miles a day, is now looking with a covetous eye on the territory surrounding the prosperous cities of southern Dakota. With- in the year past this company has built its lines into the two leading cities of central Dakota — Aberdeen, Brown county, and Watertown, Coding- ton county — and is now projecting extensions reaching nearly every city of any size in the south or southeast, two of which (the one reaching Huron, in Beadle county, and the other Sioux Falls, in Minnehaha county), will, in all probability, be completed early in 188S. In addition to these undertakings, the St. Paul, Minneapolis and Mani- toba has ironed and is operating its branch lines, graded last season ; one from Rugby Junction, on the main line, to Bottineau, the county seat of Bottineau county; one from the Minnesota state line, through Grant county, to Watertown, the county seat of Codington county, and another from Rutland, Sargent county, to Ellendale, in Dickey county. It is now busily engaged in the extension of the Park River branch, through Walsh county, to Langdon, the county seat of Cavalier county, with the promise 12 RESOURCES OF DAKOTA. of completing the same by the first of November of the present year. The Chicago and Northwestern has extended and is operating its road between Faulkton, Fanlk county, and Gettysburg, Potter county, and in- tends filling in, this season, the gap between Verndon and Groton, in Brown county. The Chicago, Milwaukee and St. Paul has completed a road from Lake Preston, Kingsbury county, to Bristol, Day county, and has ironed the grade of last season, from Roscoe, in Edmunds county, to a point several miles beyond Hillsview, in McPherson county. This company also has imview the extension, through the Lake Traverse Indian reser- vation, of the branch line now constructed sixteen miles northwest from Wilmot, Roberts county. The grade of the Chicago, St. Paul, Minneapolis and Omaha, finished in 1886, between Salem, McCook county, and Mitchell, Davison county, is now ironed and in operation. In the Black Hills, the Fremont, Elkhorn and Missouri Valley railway company is extending its road from Rapid City, Pennington county, to Sturgis, Lawrence county, and promises to run regular trains to the latter place before the expiration of the year. The Minneapolis and Pacific will be in operation from Ransom, Sargent county, through to Monango, Dickey county, by November 1, 1887, when still another connection will be finished between the railway systems oc- cupying the northern and southern territories. This extension, (the Minneapolis and Pacific), is already completed as far west as Oakes, Dickey county, and connects there with the Northern Pacific, leading north, and the Chicago and Northwestern reaching south- The Burlington, Cedar Rapids and Northern, with its terminals at Watertown, in Codington county, and Sioux Falls, Minnehaha county, seems to rest in contented mood for the present. The Illinois Central has a large force at work grading a line from Chero- kee, Iow r a, to Sioux Falls, Minnehaha county, and will make its first ap- pearance on this, the most interesting battle-ground of rival railway cor- porations, within the course of a few months. The Aberdeen, Bismarck and Northwestern has a grade finished from Aberdeen, Brown county, to Bismarck, Burleigh county, which, when ironed, (and this will be done early in 1888), will furnish the first contin- uous line, uniting north and south Dakota. The Duluth, Watertown and Pacific, (an extension of the St. Paul, Minneapolis and Manitoba), has graded a road between Watertown, in Codington county, and Huron, Beadle county, with the expectation of completing and ironing the same at an early date. This company — the Manitoba — is also pushing toward completion the grade of an extension from Willmar, Minnesota, to Sioux Falls, Minnehaha county, Dakota. RESOURCES OF DAKOTA. 13 The line is to be graded to Sioux Falls before the close of the building season, and ironed early in the spring of 1888. The grade of the Forest City and Watertown road will be finished this year, between Forest City and Hoven, Potter county, and the work of ironing and completing the track will be begun next season. The mileage of newly constructed road in Dakota, as undertaken by each company, to be completed in 1887, is given below: Name of company. Northern Pacific railway : Grand Forks to Pembina La Moure to Edgely St. Paul, Minneapolis and Manitoba railway: Mi not to Ft. Buford Rugby Junction to Bottineau Park River to Langdon Rutland to Ellendale Minnesota line to Watertown Chicago, St. Paul, Minneapolis and Omaha railway: m Salem to Mitchell Chicago, Milwaukee and St. Paul railway: Bristol to Lake Preston Wilmot extension Roscoe to Eureka x Chicago and Northwestern railway: Faulkton to Gettysburg Verndon to Groton Fremont, Elkhorn and Missouri Valley railway: Rapid City to Sturgis Minneapolis and Pacific railway: Ransom to Monango Total miles of newly constructed road in 1887 Miles of new roadconstr'd in 1887. 96 21— 117 142 38 40 49 46— 315 33— 33 73 10 26— 109 44 14— 58 59— 59 716 And the total mileage of each company in the Territory, on the comple- tion of these extensions, will be as follows: Name of company. Black Hills and Fort Pierre railway Burlington, Cedar Rapids and Northern railway... Chicago, Milwaukee and St. Paul railway Chicago and North western railway ' Chicago, St. Paul, Minneapolis and Omaha railway Fremont, Elkhorn and Missouri Valley railway...'.. Minneapolis and Pacific railway St. Paul, Minneapolis and Manitoba railway Northern Pacific railway Minneapolis and St. Louis railway Total miles of railroad in 1887 Miles of road in operation. 15 83 ,155 761 88 110 88 .037 830 40 4,20- 14 EESOUECES OF DAKOTA. The following roads have been graded, but probably will not be ironed until 1888: Name of company. ^raded. 1 * ^ Aberdeen, Bismarck and Northwestern railway: From Aberdeen, Brown county, to Bismarck, Burleigh county 160 Duluth, Watertown and Pacific railway: From Watertown, Codington county, to Huron, Beadle county I 72 Forest City and Watertown railway: From Forest City to Hoven, Potter county 30 Duluth and Willmar railway : From Willmar, Minnesota, to Sioux Falls, Minnehaha county, Dakota. Graded in Dakota Illinois Central railway : From Cherokee, Iowa, to Sioux Falls, Minnehaha coun ty, Dakota. Graded in Dakota 16 Total miles of road graded in 1887, but not ironed 301 Before the expiration of the year 1887 there will have been added to the railroad mileage of the Territory in a single season, close to one thous- and miles of new track and to what extent during the coining year Dakota will be interlaced with the iron thread of steam communication it is utterly impossible to predict, though it is quite safe to say that it will more than double the mileage built-in 1887. Dakota now has more miles of completed railroad than either California, Tennessee, Nebraska, Virginia, North Carolina, Colorado, Arkansas, Alabama, or Georgia; twice as many miles as either Massachusetts, South Carolina, Florida, New Jersey, Mississippi, or Kentucky; more than three times the railway mileage of either Maine, Maryland, West Virginia, Louisiana or Oregon; more than four times as many miles of railway as either New Hampshire, Vermont or Connecticut; thirteen times the railway mileage of Delaware, and twenty times that of Rhode Island. MANUFACTORIES. A commendable interest is being displayed by many towns in the en- couragement of manufactories. Flour mills, creameries, tow mills, pack- ing houses, wagon and carriage factories, broom factories, brick, terra cotta and stone works, plow factories, foundries, polishing works and other industries are scattered everywhere throughout the Territory and constantly increasing in numbers. The field of manufacturing is a new one for Dakota and one capable of illimitable development. With an inexhaustible supply of cheap fue- underlying every section of the north and west, with natural gas actually discovered, with artesian wells fur- nishing power for small factories at literally no expense, and the splendid water power of favored localties; with gold, silver, iron, lead, copper, tin, mica, salt, gypsum, asbestos, petroleum and many other deposits in ad- dition to the different varieties of valuable building and ornamental stones, it would be strange indeed if capital did not step in to assist in RESOURCES OF DAKOTA. 15 the development of such magnificent resources. The wonder is that the opportunities for building up prosperous manufactories as presented by a number of localities have been so long neglected. However the Territory is to be congratulated from the feet that the present year witnesses the in- auguration of an increased interest in this new source of wealth, and the hastening forward of the day when many of our food supplies and articles of commerce will have the imprint of a home factory. LIVE STOCK. The stock interests are growing quite as rapidly as other branches of industry. The natural grasses of Dakota possess nutritious and strength producing qualities not excelled in all the world, and the stock-raiser has fifty million acres of such kind of forage on which to feed his flocks. Every year notes a marked improvement in the quality of the stock- bred and numerous herds have now at their head, leaders with as fine a pedigree as is recorded in the herd-books of the country. In the older counties a large acreage is planted to corn, oats, etc., and an ever increas- ing attention is given to the raising of the best grades of improved stock. in conclusion. It is apparent therefore that the year 1887 has recorded an era of great prosperity for Dakota. The yield of the crops has been such as to astonish the world; the cities and villages are vying with each other in growth and development ; manufactories and public enterprises are being fostered everywhere, the great railway corporations of the West are in a constant strife to obtain vantage ground in the Territory and a flood r* immigra- tion is rapidly covering the vacant area of Government lands. The confidence displayed by cautious Eastern capitalists in the invest- ment of their fortunes in Dakota bonds, in Dakota lands, in railway ex- tensions, manufactories and public improvements, should convince the most skeptical that the Territory is fast assuming her position of the wealthiest, most populous, most prosperous empire of the Northwest. In-order to spread broadcast reliable information concerning the op- portunities offered by the Territory for the _ acquirement of a"home"on the finest agricultural land in the world, amid a cultured, moral and refined people, where there are schools, churches and all the "advantages enjoyed by the most 'civilized and progressive communities, — this official nanmhlet has been published under authority conferred Jby the Territorial Legisla- ture. In its pages will be found rather an extended^description of those matters which are thought to be of interest to home-seekers and inves- tors, and, while it has been hastily written and compiled under the dis- advantage of a worse than useless law governing the gathering and compi- lation of statistics, yet the facts as set forth are fairly and truthfully stated and with a desire to belittle rather than to exaggerate or deceive. 16 RESOURCES OF DAKOTA. HISTORICAL. FIRST LEGISLATION BY CONGRESS. Dakota (Indian name signifying leagued, confederated), was a part of the Territory purchased in 1803 of France by President Thomas Jefferson for the sum of $16,000,000. October 1, 1803 that part of the new purchase lying south of Arkansas was formed into the " Territory of Orleans." The remaining portion — which included the present states of Arkansas, Missouri, Iowa, Minnesota, Kansas, Nebraska, part of Colorado and the territories of Dakota, Montana, the Indian Territory and a portion of Wyoming, — became the District of Louisiana, and the governing power was vested in the governor and judges of what was then designated " Indiana Territory." July 1, 1805, by act of Congress "District" of Louisiana was designated as the "Territory" of the same name and the legislative power placed in the hands of a governor and three judges who were named by the Presi- dent and Senate of the United States. December 7, 1812, the name of the Territory was again changed, this time to "Territory of Missouri" and the power — limited in extent was granted the people residing therein, to elect a legislative body. The Territory of Michigan was created by act of June 28, 1834 and in- cluded that part of Dakota lying east of the Missouri and White Earth rivers, in addition to the present states of Wisconsin, Michigan, Iowa and Minnesota. July 3, 1836, Congress established the Territory of Wisconsin which in- cluded the eastern half of Dakota. The Territory of Iowa was organized June 12, 1838, and a part of Dakota was contained within its boundaries. March 3, 1849, Minnesota Territory was established which covered the eastern part of Dakota. Until the organization of Nebraska Territory May 30, 1854, of which it became a part, that portion of Dakota lying west of the Missouri and White Earth rivers was known as "Mandan Territory." From May 11, 1858, the date when Minnesota became a state, up to the organization of a territorial form of government, April 2, 1861, Dakota was without legal name or existence.. A bill (S. 475) " To organize the Territory of Dakota, and for other pur- poses" was introduced, on leave, in the Senate by Hon. Graham N. Fitch, December 20, 1858, and referred to the Committee on Territories. The committee was, on February 8, 1859, discharged from further consideration of the bill. RESOURCES OF DAKOTA. 17 A bill (S. 555) "To provide temporary governments for the Territories of Dakota and Arizona, and to create the office of surveyor-general in the Territory of Arizona," was reported from the Committee on Territories, Senate, by Hon. James S. Green, February 4, 1859. No action thereon was taken by the Senate. A bill (S. 562) "To provide a temporary government for the Territory of Dakota, and to create the office of surveyor-general therein, was re- ported from Committee on Territories, Senate, by Hon. James S. Green February 14, 1861; passed that house February 2(5; passed the House of Representatives March 1, and was signed by President Buchanan, March 2, 1861. President Lincoln soon after appointed the Territorial officers and, on May 27, 1861, the date of the commencement of civil history in Dakota, Governor William Jayne arrived at Yankton to enter upon the discharge of his duties. March 2, 1868, (12 stats, p. 701), an act was passed by Congress prescribing the qualifications and powers of the governor and regulating his power of veto. May 26, 1864, (13 stats, p. 92), a part of the Territory of Idaho was tem- porarily incorporated with ami made a part of Dakota. April 28, 1870, (14 stats, p. 98), the boundary line between Dakota Terri- tory and the state of Nebraska was re-defined. February 17, 1873, (17 stats, p. 464), the western boundary of Dakota Territory was re-adjusted, and a detached portion of the Territory, under former erroneous definition was attached to the Territory of Montana. LEGISLATION IN REGARD TO THE ADMISSION OF THE TERRITORY AS A STATE. A constitutional convention, composeel of delegates from nearly every county in Dakota, south of the 46th parallel, assembled at Sioux Falls on the 4th of September, 1883, for the purpose of drafting a constitution for a proposed new State. The constitution was submitted to the people (south of the 46th parallel), on the 3d of November of that year and adopted by a majority of 5,522 in a total vote of 19,150. Pursuant to an act of the Territorial Legislature approved March 9, 1885, a second constitutional convention, composed of delegates representing counties south of the 46th parallel, met at Sioux Falls, September 8, 1885, framed a second constitution, which was submitted to the people (south of the 46th parallel), November 3, of that year and was adopted by a ma- jority of 18,561 in a total vote cast of 31,791. At the same time there w r ere elected members of the Legislature, state officers and a member of Con- gress, and, subsequently, the members elect of the Legislature of the pro- posed new State met and selected two Uniteel States senators. By an act of the last Territorial Legislature, approved March 11, 1887, the question of the division of Dakota is to be submitted to a vote of the people of the entire Territory at a special election November 8, of the present year, (1887.) Following is an exhibit of the various measures introduced in Congress (since the forty-fifth session), having in view the division, the admission as a wdiole, and the division and admission of the south half of Dakota. 18 EESOUECES OF DAKOTA. • -H _ CC CO : I : I ■ : co ■j • • =2 -A CO :S i : OXX«» CO "> CO » ,(N £_ . . .O rt «H fa >> % o O 0,0.0 o o g ~ % o ^ * £ £'° ^3 PPPfefe P fe P >-, 1-5 £h g 1-3 a 3 ¥&;€&£ RESOURCES OF DAKOTA. 19 '3-f X - '*r - Sir. o ? - 2 ^d it 1 ej ;-- o © « -.= p ">. £ > >.~ ~ 03 h,2 - ° ~ ~ > g<£* H as©© hCOfi'M-^d i go © -g -r — * -£+; o g-gob ■|| 3§SSsS§|lo5 •— x .^ ■" ^ - .^ — '^ - 'S S .= -5 * "Se S ts "i § p2 © "S « — oq m'O Ortta Co fl 6^5 a ^OXMNN-tMCCN 00 t- K t" i— . i— i t— i u- rc -- L~ w u~ d 7 " H - £1 '■a c m a> e 2 c * < : x < ? -^ PS : x ■ : » "* _u 31 "* - r- x „ — X X X X - *J CO ■* i-" C4 ''- — —-" U >,>>>>|>l J *j © ei b: 2^^^ S 3 © © r « _«=:__ © S pd - ~ r; 5 3^3 ©' '" -o "S -a « a ° © - * © a e;-r «^jS| _ Sc ii"3 « 20 RESOURCES OF DAKOTA. GOVERNORS AND DELEGATES. The following is a list of the governors of Dakota appointed by the President of the United States, with the terms served by each: William Jayne, 1861-63; Newton Edmunds, 1863-66; Andrew J. Faulk, 1866-69; John A. Burbank, 1869-74; John L. Pennington, 1874-78; William A. How- ard, 1878-80; N. G. Ordway, 1880-84; Gilbert A. Pierce, 1884-87: and Louis K. Church, the present executive, appointed February, 1887. The Territory since its organization has been represented in Congress by the following named delegates: J. B. S. Todd, 1862-64; W. F. Bur- leigh, 1864-69; S. L. Spink, 1869-71; M. K. Armstrong, 1871-75; J. P. Kid- der, 1875-79; G. G. Bennett, 1879-81; R. F. Pettigrew, 1881-83; John B. Raymond, 1883-85; and Oscar S. Gifford, the present incumbent, elected in 1884 and re-elected in 1886. SESSIONS OF THE TERRITORIAL LEGISLATURE. The first session of the Territorial Legislature met at Yankton, March 17, 1862. At first the sessions of the Legislature were annual, but by act of Congress in 1869 they were made biennial, and the sessions limited in duration to sixty days. Seventeen sessions have been held in all. The Territory is apportioned into twenty council and legislative districts, represented by twenty-four councilmen and forty-eight representatives, being the maximum number of districts, councilmen and representatives permitted to the Territory under the act of Congress approved March 3, 1885. Yankton was the capitol of the Territory until 1883, when a capitol commission appointed at the preceding session of the Legislature located the seat of government at Bismarck. EARLY HISTORY OF THE TERRITORY. *The first well authenticated account of the Missouri river region, lying- bey ond the borders of the present state of Missouri, is found in the jour- nals of the expedition of Captains Lewis and Clark, under the patronage of President Jefferson's administration in 1804-5-6. This expedition^ though it gave very little scientific information touching the great valley of the Missouri, nevertheless furnished the most reliable and interesting account of the country, its inhabitants and wild game, that had then been given to the public. It also gave a very correct idea of the great river and its affluents, and was no doubt instrumental in hastening the more perfect exploration and settlement of the country. It also gave a fresh impetus to the fur trade, and pioneered the way for numerous forts and trading posts. The great British and American fur companies were the first civilized people to occupy the Territory of Dakota. The earliest of these to establish posts on the upper Missouri river was the Missouri fur company, organized at St. Louis, Mo., in 1808. At the head of this com- pany was Manuel Lisa, a Spanish gentleman, and it is likely that some of * The authority for this and following statements regarding early explorations in the: Northwest is Andrews' Historical Atlas oi Dakota. The Lakeside Press, Chicago. RESOURCES OF DAKOTA. 21 the Choteau family were also connected with it. The company established trading posts in Dakota about 1808-10. The American fur company, of which John Jacob Astor was president, was chartered in 1809. The Northwestern, another fur company, and the American were consolidated in 1811. During the war between Great Britain and the United States, 1812-15, business was wholly suspended. The Great Pacific company was organized after the war by Mr. Astor, and business operations were resumed by all the companies, whose employees penetrated all parts of the present Territory of Dakota, excepting the Black Hills. The oldest fur company in America was the Hudson Bay company, which was chartered by King Charles II in 1670. About 1811 Lord Sel- kirk, a Scottish nobleman, was granted by this company a large tract of land lying on both sides of the Red River of the North, and extending as far south as the mouth of the Red Lake river. Lord Selkirk built a fort at Pembina, a short distance south of the pres- ent International line, about 1812. The first settler in this region was a French trader, who settled at Pem- bina about 1780. The authority for this statement is Mr. Keating, the historian of Major Long's expedition, which visited the locality in 1823 and found the trader still living there. This was the first actual settle- ment by white men within the present limits of Dakota. Lord Selkirk's fort remained at Pembina until 1823, when rinding it was on the American side of the boundary, it was torn down and mostly removed to the British side. The Columbia fur company was organized in 1822 among individuals formerly in the employ of the Hudson Bay company. Their principal establishment, or trading post, was on Lake Traverse at the head of the Red River, where Major Long found them in 1823. The Northwest and Hudson Bay companies, under a consolidated arrangement made in 1821, explored and trafficked on the Upper Missouri and Yellowstone rivers. In 1826, a company called the Rocky Mountain fur company, began sending trading expeditions up the Missouri river. In 1832 the old Amer- ican fur company of John Jacob Astor became the dominant company in the Northwest. Under this company Forts Cedar, George, Lookout and others were constructed, and the fur trade became a permanent business in the Missouri valley. Several trading houses were also erected on the Dakota (James) river by a company of which J. Rencontre was a member. About 1829, Pierre Choteau of St. Louis, built Fort Pierre on the west bank of the Missouri, some four miles above the present site. The first steamers to ascend the upper Missouri, as near as can be as- certained, were the Yellowstone and Assiniboine, which came up under the conduct of Pierre Choteau, about 1830. Previous to this the business of the river had been carried on in canoes and barges, or pirogues. 22 RESOURCES OF DAKOTA. In 1839 Fremont and Nicolet ascended the Missouri on the fur com- pany's steamers to some point in Dakota, and from thence passed over- land to the valley of the Dakota (James) river, and are said to have as- cended the latter stream and visited Devils Lake, though there is no well authenticated account of the trip recorded. Catlin, the famous Indian de- lineator, visited the country in 1841. From that date military and private expeditions were numerous. The United States Government established a post at Fort Clark, below the mouth of Knife river, as early as 1808, followed closely afterward by the construction of forts at many points, principally along the Missouri river. The forts and posts at first established were partly military and partly trading posts — the former established by the United States Government, and the latter by the great fur companies. FIRST SETTLEMENT. The first land in Dakota obtained of the Sioux Indians, was at the treaty of Traverse de Sioux in 1851, by which the Indians ceded a large region in Minnesota and a tract of country along the left bank of the Big Sioux river and the southwest side of Big Stone lake, including the cites of Sioux. Falls, Flandreau, Brookings, etc., covering substantially the strip of country lying between the Big Sioux river and the Minnesota line. In the same year the legislature of Minnesota Territory, (which in- cluded at the time all of Dakota east of the Missouri river), divided that territory into nine counties, Dakota county covering all the region lying between St. Paul and the Missouri river, and constituting the sixth coun- cil district entitled to two councilmen and one representative in the Min- nesota legislature. In the fall of 1855, a United States force of 1,200 men, under General W. S. Harney, marched from the Platte river to Fort Pierre, where they en- camped for the winter. Accompanying this expedition were Captain (afterward General) Nathaniel Lyon, who fell at the battle of Wilson's creek in 1861; Captain J. B. S. Todd, the first Territorial delegate in Con- gress, and Captain Gardner, afterward a general in the Confederate army . Old Fort Pierre, erected by Pierre Choteau, of St. Louis, about 1829, was taken possession of by the United States troops, the Government pay- ing Choteau a considerable sum for his improvements. Captain Sully was ordered from Fort Abercrombie to Fort Pierre, and marched across the country with two companies of infantry, and occupied Fort Pierre un- til 1858, when the place was abandoned by the Government, Captain Sully removing with his command to Fort Ridgely. Old Fort Lookout, near Chamberlain, was occupied by General Harney in 1856, but in the spring of 1857 he selected the site of Fort Randall, which was erected and occupied in June of that year. Captain Lyon held Fort Lookout until 1858, when the place was abandoned. The first attempt at settlement in southern Dakota was made at Sioux EESOUKCES OF DAKOTA. 23 Falls, in the fall of 1856, by an organization called the Western town com- pany, of Dubuque, Iowa. The men who ventured to commence a settle- ment were ordered off by the Indians, and returned to Sioux City, Iowa. In December following a second attempt was made by members of the same company, who took possession of 320 acres of land around the falls. In May 1857, other representatives of the company again visited Sioux Falls, and began the erection of a small stone house near the upper fall. About the same time the Dakota land company, chartered by the Min- nesota legislature, made a claim to 320 acres of land immediately south of the land held by the Western land company. The members of the Dakota land company left St. Paul in a steamer, in May 1857, and pro- ceeding to New Ulm on the Minnesota river, traveled thence overland to Dakota, striking the Big Sioux river in Brookings county, where they lo- cated the town of Medary, named for the governor of Minnesota. Jour- neying down the river they located and named Flandreau, in honor of Judge Flandreau, of St. Paul, and then pushed on to Sioux Falls, where they located land, as before stated, and named the place Sioux Falls City. In July of that year an uprising of the Sioux Indians compelled the evacuation of all the settlements on the Sioux river. In December 1857, the governor of Minnesota appointed the first ofn cers of Big Sioux county, now constituting the county of Minnehaha Dakota. In June 1858, the Indians a second time drove the settlers out of the upper valley of the Sioux. On the 19th of April, 1858, a treaty was negotiated, by which the Yank- tonnais tribe of Sioux Indians ceded all their lands east of the Missouri river excepting the present reservation in Charles Mix county. From this date settlers came in rapidly, especially in the region border- ing on the Missouri and Big Sioux rivers. The autumn of 1862 witnessed the blood)- outbreak of the Sioux Indians, which resulted in the dreadful massacre at New Ulm, 'Minnesota. The inhabitants of all the settlements in southern Dakota fled to Yankton, abandoning their crops, herds and dwellings, in their haste to reach a place of refuge. The outbreak proved to be of short duration, and the settlers soon began to return to their homes. In 1861 the War Department authorized the governor of the Territory to raise two companies of volunteers for the war. These two companies officered by Captains Nelson Miner and William Tripp were stationed the following winter among the settlements of southern Dakota. In the summer of 1863 an organization known as the "New York col- ony" was effected at Syracuse, New York, which delegated Hon. James S. Foster, now of Mitchell, to personally visit the West and select locations for the colony. In accordance with Mr. Foster's recommendations, about one hundred families left New York in the spring of 1864, and settled at various points in the Missouri valley between the Big Sioux river and Bon Homme, southern Dakota. 24 RESOURCES OF DAKOTA. The assessed valuation of the Territory in 1865 had grown to $158,903. During the years 1867-8 the population of the Territory increased rap- idly, and many new colonies were organized. A railroad was completed to Sioux City, Iowa, near the Dakota line, in 1868, and the rush of immi- gration which followed was so great that at the close of that year, the population of the Territory was estimated at 12,000. By the treaty of April 29, 1868 the Sioux were re-located on their pres- ent reservation west of the Missouri— and troubles with the Indians, which had so often threatened the early settlements east of the river with extinction, were forever at an end. The first telegraph line in the Territory was built from Sioux City to Yankton in 1870. Railway construction was carried on extensively in 1872, and in 1873, the Sioux City and Yankton road was completed to the latter place. In 1874, gold was discovered in the Black Hills by General Custer's ex- pedition. Under an agreement with the Sioux Indians, ratified February 28, 1877, the Black Hills country was relinquished to the United States and immediately taken posession of by a throng of hardy pioneers, miners and ranchers. The growth and development of Dakota during the decade since 1877, as fully detailed in the statistical tables and comparisons making up the succeeding pages of this pamphlet, forms one of the most marvelous epochs in the history of the settlement of the West. RESOURCES OF DAKOTA. 25 GEOGRAPHY OF DAKOTA Dakota is situated between the meridians of 96° 25' and 104° 5 / longi- tude west from Greenwich, and between the parallels of 42° 28' and 49° north latitude, and is located on the northern line of the Republic, about midway between the Atlantic and Pacific oceans. Its extreme length north and south approximates 430 miles, and east and west 385 miles. An official work on the public domain, published in 1888, by authority of Congress, estimates the present area of Dakota at 150,932 square miles or 96,596,480 acres. Dakota is greater in area than either the kingdoms of Norway, Great Britain and Ireland, or Italy; more than twice the size of either England and Wales, or Turkey in Europe; over four times the size of Portugal and nearly live times greater than Ireland or Scotland, and would make ten Denmarks or Belgiums. The distance from Yankton, on the southeast boundary, in a straight line to Pembina, on the northern boundary, is nearly as far as from Chi- cago to Memphis, or from New York to Raleigh, N. C, or from "Washing- ton to Ottawa, Ont. To better comprehend the vastness of Dakota's landed possessions, it may be stated that the states of Maine, New Hampshire, New Jersey, Vermont, Connecticut, Rhode Island, New York, Delaware, Maryland and Massachusetts could all be placed within her boundaries, and yet there would be room for another state as large as Massachusetts, which, if added, would still leave a place for two additional states the size of Connecticut, and with these added, there remains room for two more Delawares and six Districts of Columbia— and still the area of Dakota would not be covered. 26 RESOURCES OF DAKOTA. TABLE SHOWING THE AREA OF DAKOTA In comparison with that of each state and territory of the Union. 28 NEW YORK, 27 NORTH CAROLINA, ALABAMA, 25 ARKANSAS, 24 FLORIDA, 23 WISCONSIN, 22 IOWA, 21 ILLINOIS, 20 MICHIGAN, 19 GEORGIA, RANK. STATES. SQUARE MILES. ACRES. 48 DISTRICT OF COLUMBIA, 60 38,400 47 RHODE ISLAND ~1 1,085 694,400 46 DELAWARE, I 1,960 1,254,400 45 CONNECTICUT, I~ 4,845 3,100,800 44 NEW JERSEY, ■ 7.455 4,771,200 43 MASSACHUSETTS, ^T 8,040 5,145,600 42 NEW HAMPSHIRE, 41 VERMONT, 11 9,005 9,135 5,763,200 5,846,400 40 MARYLAND, ■ 9,860 6,310,400 39 WEST VIRGINIA, 38 MAINE, ■ 24,645 29,895 30,170 15,772,800 19,132,800 37 SOUTH CAROLINA, mm 19,308,800 36 INDIANA, ma 35,910* 40,000 22,982,400 35 KENTUCKY, ~~SiSSI 25,600,000 34 VIRGINIA, Kiln 40,125 25,680,000 33 OHIO, t\v-'-J 40,760 26,086,400 32 TENNESSEE, in 41,750 26,720,000 31 PENNSYLVANIA, 30 LOUISIANA, — ■ 1 44,985 45,420 28,790,400 29,068,800 29 MISSISSIPPI, 46,340 29,657,200 18 WASHINGTON TER. 17 MISSOURI, 16 INDIAN TER., 15 NEBRASKA, 14 MINNESOTA, 13 KANSAS, 12 UTAH, 11 IDAHO, 10 OREGON, 47,620 48,580 51,540 53,045 54,240 14,450 >5,475 1,000 30,476,800 31,091,$ 32,985,600 33,948,800 34,713,600 34,848,000 35,504,000 35,840,000 K§7,430 36,755,200 HJ8,980 37,747,200 E&880 42,803,200 E|,735 43,990,400 Sg830 44,691,200 Sj.85 48,758,400 1$05 50,691.200 Kfao 52,288,000 52.601,600 53,J15,600 60,518,400 62,448,000 3 DAKOTA, 2 CALIFORNIA, 96,596,480 99.827.200 RESOURCES 01 DAKOTA. 27 COMPARATIVE TABLE Showing the area of Dakota in square miles as also that of some of the Foreign Governments. Rank (rovernment. Squa re Miles, 1 MONACO, I 6 2 ANDOKEA, ■ 198 3 MONTENEGRO, EHi 1,770 4 BELGIUM, ■■ 11,373 5 EASTERN ROUMELIA, ■Btt 13,500 6 DENMARK, HHffi 14,553 7 SWITZERLAND, esehs 15,233 8 GREECE, HBBH) 19,941 9 NETHERLANDS, 10 SERVIA, 11 BULGARIA. 12 bosn: 13 IRELAND. 14 PORTUGAL, 15 ROUMANIA, 16 ENGLAND & WALES, 17 TURKEY IN EUROPE 20,527 20,850 24,360 28,125 31,874 i,510 45,642 62,028 18 ITALY 114,296 19 GT. BRIT. & IRELAND 20 NORWAY, 21~DAKOTA, 22 SWEDEN, 23 SPAIN, 120,879 24 FRANCE. 25 GERMAN EM. A I STRIAN EM 204,091 240,943 TOPOGRAPHY. The general topography of the Territory is that of a vast undulating plain, which covers about four-fifths of its surface. The great Plateau du Coteau du Missouri, of the French explorers, occupies a belt traversing the Territory diagonally from the northwest to the southeast. This is not the high dividing ridge that it was formerly supposed to be, but simply a vast elevated plain, occasionally broken by low hills. A somewhat simi- lar plateau, but much less in extent, lies between the Minnesota line and the valley of the James river. The country west of the Missouri river, (the largest part of which is contained within the boundaries of Indian reservations), has much the same character, although more broken by hills and buttes, and with the advantage of a greater number of streams, which are fringed with con- siderable timber. " Topographically Dakota may be divisible into two parts — eastern and western. The portion west and northwest of the Missouri river is undu- 28 RESOURCES OF DAKOTA. Iating. As we approach the southwest line it is rugged and mountainous. Here are found the rich mineral lands of the Black Hills. The great portion east of the Missouri, or the settled, cultivated part of Dakota is chiefly a vast plateau or plain, generally with but little native timber. The surface is smooth, even on the undulating portions, is cov- ered with a luxuriant growth of grass, and abounds in lakes and rivers, many more than are apparent on the maps. Strange as it may seem, the lakes are often on the highest grounds. This abundance of moisture would suggest swamps, but a team can be driven anywhere at all seasons, regardless of established roads. The lakes are chiefly where the water does not drain off. Again, the marsh wire-grass is not met, only the up- land varieties, chiefly the bunch, blue-joint and the buffalo grasses. Like the pampas of South America, the lands furnished an abundance of graz- ing for the vast herds of buffalo that roamed over Dakota but a few years ago. A boulder here and there on the surface is encountered; otherwise there are no rocks or strata of rocks apparent, even on deep digging, with the exception of one or two localities. The surface soil is composed of two or three feet of black loam (humus), then several feet of brown, clayey, gravelly soil, (hard pan). Beneath that, pockets of gravel and sand are met, and finally a layer of deep-blue clay is encountered, some- times many feet in thickness, and again gravel and sand. In some cases well-diggers have come across the stumps of trees (cedar) thirty feet be- low the surface. The water in some of the lakes and rivers is slightly al- kaline, and occasionally even brackish. Hard water is generally due to the large proportion of carbonate of lime, but, in addition to this, Dakota soil water, (when alkaline), contains sulphate of soda, sulphate of mag- nesia, sulphate of lime, and common salt, all of which give it a brackish taste. The soil, however, for this very reason, is peculiarly adapted to the growth of wheat, for which Dakota has become so famous." — [" Dakota From a Scientific View"; Dr. T. C. Duncan, Chicago. MOUNTAINS AND HILLS. Properly speaking, there are only two mountainous regions in Dakota, known as the Black Hills and Turtle Mountain. The Black Hills, located in the extreme southwestern part of the Territory, cover an area in Da- kota equal ;to about 40 by 80 miles, or equivalent to 3,200 square miles. The Turtle Mountains of Bottineau and Rolette counties in the far northern portion of the Territory are a range of high hills dignified by the name of mountains, rising a few hundred feet above the prairies. They cover an area of about 20x40 miles or 800 square miles. The highest point of the Black Hills, Harney Peak, reaches an altitude of 8,200 feet above the sea, and the average elevation of the Hills region is nearly 6,000 feet, or from 2,500 to 4,700 feet above the surrounding plains. The Turtle Mountains are surmounted by only one or two high peaks — notably, Butte St. Paul and Bear Butte, which are elevated some 700 feet above the surrounding countrv, and 2,300 feet above the sea. RESOURCES OF DAKOTA. 20 Both the Black Hills and Turtle Mountains are covered with a consid- erable growth of timber, the former principally with pine and the latter with oak, aspen, birch., etc. The Wessington and Ree Hills in Hand county, are quite prominent elevations, as are also the Bijou Hills in Brule county. GEOLOGY. The geological structure of Dakota covers a wide range of formations, from the Archaean of the Black Hills to the fresh water Tertiary and Quartenary of the great plains, and the Missouri valley. Scientists say that Dakota lay directly in the path of a great continental glacier, which in its passage eroded and ground down the loftiest mountains and the flintiest of rocks and carried the debris, according to its composition and specific gravity, to greater or less distances. This erosion of the ancient rocks and mountains must have been enormous to have produced such a vast accumulation of drift material, as is found overlaying the plains of Dakota. Professor Denton, of Massachusetts, a distinguished geologist, has aptly described the causes which led to the formation of the deep and rich soil of the Red River valley in the following words: "When the cold of the glacial period gave place to the present climate, the indications are that the change took place instantaneously, and the great ice sheet then cov- ering this northern region — in some places a mile or more in thickness — was" (by a new inclination of the earth's axis to the plane of its orbit), " suddenly introduced to a temperate climate. Melting in the hot sum- mer suns, it produced a flood, the effects of which are observable to the geologist, from north Minnesota to the Gulf. But such a body of ice melted not in one or a dozen summers. For many years lay the great ice- field to the north, preventing the passage of waters' in the direction the general slope of the country here would have led them, and thus, as far south as the slope of the land would permit, a lake existed. At the bottom of the lake, mud was continually being deposited, produced by the ground down Silurian, Devonian and Cretaceous beds lying to the north, over which the ice still for many years continued to move, bearing masses of their earthy substances. Boulders, gravel, etc., are covered deep be- neath the lake mud, and that mud is now the soil of the country, admi- rably adapted to the production of grain best fitted to build up the physi- cal system of man." And as the soil of this section is the drift and alluvial deposit of glacial action, just so was the soil of the great Missouri plateau, the James river valley, and, in fact, every foot of the Territory formed. The granitic boulders carried down by glacial streams from the Archsen regions of Minnesota and Canada are found cropping out along the slopes of the bluffs bordering the James and east bank of the Missouri rivers, and are frequently discovered in boring wells 40, 60 and 100 feet beneath the surface, giving some idea of the depth of the drift deposit. Through- out the country east of the Missouri, these granitic boulders are common; 30 RESOURCES OF DAKOTA. west of the river they are fewer and smaller in size, and finally, within a distance of a hundred miles, disappear altogether, showing that glacial action was confined somewhat to the eastern half of the Territory. This theory is very forcibly demonstrated at Pierre, where, on the east bank of the Missouri, the hills adjacent to the river are crowned with boulders of all sizes, while immediately across the stream not a boulder is to be found. Prof. Denton speaks of the gradual disappearance of the indications of glacial action west of the Missouri river, as follows: " From the Missouri river for about sixty miles west on the line of the Northern Pacific, we find boulders of granite, gneiss and quartzite dimin- ishing in size and number as we go west, till at the distance named they disappear from the hills and are found only in the valleys and beds of the streams. In the valley of the Green river, 100 miles west of the Missouri at Bismarck, I found the last drift fragments where they had been floated on ice cakes and dropped, and beyond this westward for eighty miles, and probably on to the Rockies, no vestige of drift nor indications of glacial action exists. The western part of the United States, except in the high mountain regions, was not covered with ice during the glacial period any more than was northern Asia. The boulders on the hills west of Mandan, (near the Missouri where the Northern Pacific crosses it), and those scat- tered over the country east of Bismarck, were dropped by floating ice- bergs passing down the Missouri river, whose waters then resembled a sea. For boulders to have passed over that nortion of Dakota, the waters must have stood 500 feet higher than the nresent level of the Missouri, and they then covered a breadth of more than 100 miles." At a later period, during the post-glacial days, while the vast ice-field was melting away, Dakota is supposed to have been covered by a great inland sea, through which flowed the Missouri and other streams, bring- ing down the sediment formed by the northern glaciers grinding up the rocks around their head-waters. This sediment came from the disinte- grated and pulverized rocks of the Cretaceous and Tertiary formations, which are generally soft, porous and friable. Subsequently, by the deep cuttings of the streams, the waters of this great inland sea were carried off to the ocean and the Dakota plains appeared. The surface over every part of the Territory has been greatly modified since the glacial period by the action of flowing water. The greatest effect has been in the Black Hills region, where the cuttings and erosions reach several thousand feet. The valleys of the Missouri and other streams have all been cut out since the vast blanket of slowly-moving ice covered the land. It is also quite probable that several fresh-water lakes have existed since that period, besides the great lake of the Missouri valley whose waters have been drained off by the cutting of the streams. The alkali with which the soil of the Dakota plains is impregnated, has been derived, in great part, from the ground-up rocks of the Cretaceous and Tertiary periods, which contained quantities of imperfect coal, salts, sulphuret of iron, and other chemical ingredients. RESOURCES OF DAKOTA. 31 Some have a theory that the coal of the Tertiary formation once ex- tended over nearly the whole of Dakota, and that it has been burned out, leaving the soil impregnated as now found. This theory is not well sup- ported, however, by tangible evidence. *The natural history of the peculiar formation of Dakota is, as near as geologists can now unravel the mystery of the continent formation, sup- posed to be as follows: The infant continent of North America, as it rose above the primeval waters, was supposed to be in the shape of a rough triangle, with one extremity reaching beyond Winnipeg and the other away off beyond Quebec, while the junction was about the union of lakes Superior and Huron ; at least the oldest discovered, or Laurentian rocks, are along those lines. As the portions to the south and west rose grad- ually out of the prehistoric ocean, we can understand that this section contained the wealth of the early sediment. * Geologists have arrived at the conclusion that the entire area of the United States and territories was, during the lower Silurian age,the bed of a comparatively shallow sea.' — [Winchell.] Finally the Rocky mountains and the Alleghenies were thrown up, walling in the glaciers that subsequently mowed down from the upheaved north, grinding oft tne fertile portions of the new continent and depositing this with other drift r"Ter this Dakota region, which would account for the trees being buried under clay, gravel, sand, soil and other debris. This whole Mississippi valley was, as it is sup; osxl, again sub- merged at the close of the glacial era, and again to rise, and was, until quite recently, a series of shallow lakes. At least that is the recent view of the origin of the many prairies. Into these lakes the water of the sur- rounding country was drained. The sediment, broken rocks, glacial de- bris, and rank vegetation of the long ages, gave a saline character to these lake waters. Where they were shut in, like Salt Lake, they became more brackish than the ocean. ' Sea water may be regarded as the accumula- tion of all the surface drainings of the earth.' — [Brand's Chemistry.] Dakota, at this time, was undoubtedly a vast lake, with, at present, unde- fined limits. It doubtless extended from the north to the extreme south of the Territory, even into Iowa and Nebraska, and from central Minne- sota, on the east, to the Missouri river or beyond. This vast lake received the wealthy washings from virgin land all around, until finally the water became decidedly brackish. The saline ingredients underwent many changes, but much was deposited in the sediment at the bottom. It is well known that water, especially the saline, forms a precipitate. The lake began to overflow and the Dakota, or James river, to the south, and the Red River to the north, drained this vast expanse, and luxurious grasses took possession of this lake bed with its heavy deposit of organic matter, and it became the home of the buffalo, Indians and prairie fires. Such, in brief, seems to be the natural hi st ory of this won derful section. * "Dakota From a Scientific Point of View"; Dr. T. C. Duncan, Chicago. 32 RESOURCES OF DAKOTA. SOIL. The Department of Agriculture, Washington, during the year 1885, in- vestigated at some length the chemical composition of different soils, with reference to their fertility, and believing the agriculturist will find in the chemist's report a fund of information about soils in general, and especi- ally as regards the kinds of crops adapted to the prairie soil of Dakota, space is given to the following summary: The chemical composition of the soil, when taken in connection with its physical state and the climatic condition of the locality, is a guide to scientific agriculture, which cannot be neglected. All soils are the results of the natural disintegration of the rocks by atmospheric agencies, mingled with decayed vegetable and animal matter in greater or less proportion. Soil is a mixture of sand, either quartzose or feldspathic, clay, carbonate of lime and humus, or organic matter, and on the preponderence of one or more of these constituents the usual classification of soils are based. Whatever their composition and texture, soils are, from a geological standpoint, mainly of two sorts, soils of disintegration and soils of trans- port. Under the former are comprehended such as arise from the waste and decay of the immediately underlying rocks, the limestones, trap, granites, and the like, together with a certain admixture of vegetable and animal debris, and which are directly influenced in their composition, texture and drainage by the nature of the subjacent rocks from which they are derived; under the latter are embraced all drift and alluvial materials, such as sand, shingly debris, miscellaneous silt and clay, which have been worn from other rocks by atmospheric agencies and trans- ported to their existing positions by winds, waters or ancient glacier actions. All exposed rocks break up, in course of time, under the continued action of atmospheric agencies, however hard or refractory they may be. From the hardest granites, basalts and lavas to the softest limestones and marls, all are undergoing this disintegration and the soils to which they give rise will vary in depth, composition and texture, according to the softness and mineral character of the rocks and the length of time they have been subjected to these agencies. The rocks of which feldspar is RESOURCES OF DAKOTA. 33 one of the constituents are the origins of the clays and potash,, which are met with in all arable soils. Feldspar is a silicate of aluminium and potassium, which in disintegration forms a clay or silicate of aluminium, and a silicate of potassium. The primitive and igneous rocks yield soils rich in potash and the fossiliferous rocks those rich in phosphoric acid. From an agricultural standpoint, the soil, which is the natural storehouse and laboratory whence plants derive their supply of food, should present different qualities which, according as they are more or less developed, exert a considerable influence upon its fertility ; it should be firm enough to afford a proper degree of support for the plants that grow on it and yet ]oose enough to allow the delicate fibers, of the rootlets to extend them- selves in all directions in search of the food of which they are in need. It must be of such a texture as to allow the free access of air, without which plants cannot live; and it must be close enough to retain, for a considerable time, the water which falls on it, and yet porous enough to allow the excess to drain away. In this respect the nature of the subsoil and the depth of the surface soil are both important. When a soil rests immediately upon a bed of rocks or gravel, it will naturally be dryer than when it rests on clay or marl. On the other hand, a clay subsoil may be of great advantage to a sandy soil, by enabling it to retain moisture longer in dry weather. Those soils are best adapted to agriculture which consist of a mixture of sand with a moderate quantity of clay and a little vegetable matter. The ammonia floating in the atmosphere is continually being" washed into the soil, carried into it by the rains. The clay, oxide of iron, and the organic matter contained in the soils, perform the important function of absorp- tion. This property of clay may be one of the reasons why clay lands are more suitable to wheat than are sandy soils. The amount of moisture re- tained by a soil, is generally in direct ratio to its contents of organic matter and its state of division. A proper degree of fineness in the parti- cles of the soil is very important to obtain, especially if it is subjected to drought. During dry weather plants require a soil that is both retentive and absorptive of atmospheric moisture and that soil which has this faculty will evidently raise a more vigorous growth than one without it. The materials which are most influential in soils may be arranged in the following order, when this condition of retaining moisture is considered: — Organic matter, marls, clays, loams and sands. The action of rain carries the soluble ingredients which the plants re- quire to their roots and supplies them with the necessary moisture. The soil however, must be permeable enough to let the excess water drain away. The amount of food taken from the soil by wheat is given in the follow- ing table from the " Chemistry of the Farm '": 34 RESOURCES OF DAKOTA. WHEAT. The weight and average composition of wheat in pounds, per acre (R. Warrington). Weight of crop— d Z '- 2 -i "3 1 \i \ I 1 1 1 ; i Bh x h! f-- Pk O 3 Dry. Total pure a Lbs ' Lbs Lbs Wheat, grain (30 bushels)..,.... 1,800 1,530 31 Straw 3,158 2,653 158 Lbs Lbs Lbs Lbs Lbs Lbs Lbs Lbs Lbs. 9.7 .9 1.0 3.7 14.3 .2 .5 18.2 2.: 9.2 4.0 8.4 1.7 110.6 Total crop 4,958 4,183 189 45 7.8'27.9 3.410.2 7.7 22.7 1.9 111.1 Iii general, we may say that cereal crops apparently possess a capac- ity for feeding on silicates not enjoyed by other crops, and contain a less amount of nitrogen than either the root or leguminous crops; neverthe- less they respond the most readily to nitrogenous manures. The amount of phosphoric acid is the most constant of all the constituent of crops, being concentrated in the grain. The root crops contain a large amount of potash, and are the most exhausting to the soil in consequence; they take up more nitrogen than do the cereals, besides other ash constituents, as phosphoric acid. Leguminous crops contain about twice as much ni- trogen as do the cereals, and the potash and lime occurs in large propor- tions. Silica is nearly absent. They respond most readily to potash manures. The growth of forests is far less exhausting to a soil than are most ordi- nary farm crops, especially where the leaves from the trees are left to manure the ground by their decay. Soil consists of an organic and of an inorganic or mineral part, the for- mer derived from the decay of plant-life for many ages, together with the dung and remains of animals, and the latter arising from the weathering of the rocks. The organic matter varies in different soils, being most deficient in sandy soils and poor clays, and even in very fertile lands occurring only in small quantities. In the famous black soil of Russia, which is found in the provinces of the Ural mountains, and in those that border them, it varies from 5 to 12 per cents In some of our own prairie soils the amount is nearly as high. In leaf mold it occurs considerably higher, and in peat more than 50 per cent., very often. From its dark color it is a good ab- sorbent of heat, its own specific heat being much above that of the soil generally. It is hygroscopic and greatly increases the water-holding power of sandy soils; besides, it has the power of absorbing and retaining ammoniacal salts. By its decomposition it forms a source of carbonic acid, which is readily absorbed by plant-life. The mechanical condition of a soil is much improved by its presence when in moderate quantities, but when present in excessive amount it acts injuriously by deoxidizing ferric RESOURCES OF DAKOTA. 35 salts, and in other ways. [Versuchs Stationen Organ, vol. xiv. pp. 248- 300.] The inorganic- or mineral portions of the soil is, with the addition of alumina, composed of the same substances as make up the inorganic por- tion of plants, and which form their ashes when burnt. The mineral soil- constituents include the following substances: ca,Si0 2 . Potash, KoO. Alumina, A1 2 3 . Soda, Na 2 Q. Lime carbonate, CaCo,. Magnesia, MgO. Ferric oxide, Fe 2 3 . Chlorine, CI. Phosphoric acid. r_.0.-,. Sulphuric acid, S0 3 (Phosphoric anhydride.) (Sulphuric anhydride.) These exist in very different proportions in different soils. The first three, sand, clay and lime, represent more than 90 per cent, of the sub- stance of most soils, and as one or the other predominates the soil is said to be sandy, clayey, or calcareous. The most active constituents of the soil, phosphoric acid, and the two alkalies, potash ami soda, occur in very small quantities, as do the other and less important constituents, mag- nesia; chlorine, and sulphuric acid. Silica exists in different proportions in v tils, mostly in an insol- uble state, and that, most largely, in the poorest sandy soil-;; fertile soils cor.' ally a very small quantity of it in a soluble form. Sandy soils contain from 70 to 00 per cent, of silica; even stiff clay soils from 60 to 70 per cent.; and calcareous or lime soils and maris from 20 to 30 per cent. Its value, as a source of plant food, consists in being in the form of solu- ble silicates. In its insoluble state, like quartz sand, its action is nearly mechanical, making the soil lighter for cultivation. Those soils, derived from rocks of which feldspar is one of the constituents, will contain some silica in a. soluble form, whilst those derived from quartzose rocks will contain it in the insoluble state. The hyd rated silica, in the analyses, represents that which is gradually available for plant food. Alumina, or clay, is a silicate rjf aluminium, and it is derived from the disintegration of feldspathic rocks and other similar silicates; if absolutely pure it would furnish nothing for plant food; as, however, this is seldom the case, it furnishes a supply of potash frequently in considerable quan- tities, ("'lay has the important property of absorbing and retaining phos- phoric acid, ammonia, potash; lime, and other substances necessary for plant food. Clay soils contain on an average from 6 to 10 per cent, of alumina. In sandy soils it varies from 1 to -1 per cent., and in marls, cal- careous soils, and vegetable molds from 1 to 6 per cent. The presence of alumina in the soil is purely mechanical, as it is never found in the mineral portions of plants, and the larger the precentage of it present the more difficult the soil becomes to cultivate, offering a great- er or less resistance to the implements of tillage. The lime or calcareous matter generally occurring in the state of carbon- ate varies in soils from about 90 per cent, and under in limestones and 36 RESOURCES OF DAKOTA. marls, to mere traces in some other soils. Clays and loams generally eon- tain from 1 to 3 per cent, of the carbonate. Less than one per cent, may be regarded as a defective quantity. In the lighest sandy soils the per- centage of lime should not fall below .100, in clay loams not below .250, and in heavy clay soils not below .500. Where a soil is deficient in lime, the little there is of it is present in combination with the organic acids, and is more abundant on the surface than in the subsoil. It preserves the particles of clay in a separate coagulated condition, and thus allows them to exercise their absorbent powers on various salts, which other- wise would escape their action. It also promotes the decomposition of vegetable matter and the formation of nitrates in the soil. Most green crops are often subject to disease when grown on soils defi- cient in lime, even when they have been well manured. Up to a certain stage, the cereal or other crops appear to thrive well, but as the season advances they sustain a check and yield a poor harvest. This is espec- ially the case in poor sandy soils, and a good dose of lime or marl, followed by barnyard manure or guano, has a most beneficial effect. By this means the valuable portion of the manure or guano, the ammonia, pot- ash, and phosphoric acid, are retained in the land, whilst the others com- bine with the lime and are gradually washed out. Ferric oxide is found in all soils, and causes the reddish color so very common in a great many of them. To its presence is chiefly due the re- tention of the phosphoric acid, an insoluble basic phosphate of iron being produced. On its state of oxidation depends its favorable influence on the soil, that of ferric, sesqui or peroxide, better known as the red rust of iron, being the most suitable. In its less perfectly oxidized forms, which are, however, soluble in organic acids that exist very often in the subsoil, it becomes peroxidized on exposure to the air. Its action is both physical and chemical. The preference of farmers for " red land " arises from their experience of its beneficial action in the soil. From 1.5 to 4 per cent, of ferric oxide is ordinarily found in soils but slightly tinted. Ordinary ferruginous loams vary from 3.5 to 7 per cent.; highly colored "red lands " have from 7 to 12 per cent., and occasionally 20 per cent, and more. The efficiency of the ferric oxide depends upon its mechanical condition; when incrusting the grains of sand or occurring as nodules, whilst the chemical analysis may show a large percentage of it present, it exerts little or no influence upon the soil, but when in a state of fine division these advantages are realized. Soils containing a large percentage of ferric oxide have generally a low percentage of organic matter, but, notwithstanding, are, as a rule, very fer- tile. In clay lands, especially, its presence is very beneficial as tending to make them easier for tillage ; its color tends to the absorption of heat and of oxygen. Such soils, however, suffer from floods or bad drainage, the ferric oxide becoming reduced under such circumstances to the ferrous state. Phosphoric acid m contained in all good soils, but in very small quantities RESOURCES OF DAKOTA. 87 when compared with the other principal ingredients, and exists in com- bination with lime, iron, and alumina, phosphate of lime being its most common form. In general, even in the most fertile soils, it. is found in very minute quantities, on an average less than one-iialfper cent.; in clay lands this may rise to 1 per cent. Its value in fertilizers depends on its state of combination, whether it is soluble and immediately available for plant food as the superphosphates, or slowly soluble like the lime phos- phates,forming a reserve store of food for the future. It occurs in all soils that have been formed from such rocks as the granites, gneisses, lime stones, and dolomites, which contain it without exception; volcanic soils possess it in large quantities, whilst alluvial soils and those lands that are periodically swept by floods, are much poorer. Soils containing less than .05 per cent, of it will be sterile and unfertile, as a general rule, unless accompanied by a large amount of lime. Potash. — All soils suitable for cultivation contain potash in an available form, arising from the disintegration of feldspathic and other rocks. In the majority of cases the natural supply of the soil is sufficient to furnish to the plants the potash of which they are in need; a soil containing .125 per cent, should furnish potash enough for a century, without its being necessary to add to the manures used on such soils any salt of potash. Besides this available potash, the soil often contains very considerable quantities of this element which the acids do not attack, and which form the reserve for the future supply of the plants. The quantity of potash varies in the different soils from the merest traces up to 1 and 2 per cent. Sandy and peaty soils and marls are gen- erally deficient in this alkali, whilst soils rich in alumina are, with sonic exceptions, also rich in potash. It exists in the soil in combination with silica, forming a silicate which is somewhat soluble in water. Heavy clay soils and clayey loams, vary from .8 to .5 per cent. ; lighter loams, from .45 to .30 per cent.; sandy loams, below .3 per cent., and sandy soils of great depth may contain less than .1 per cent v consistently with fertility } de- pending on the amounts of lime and phosphoric acid with which it is as- sociated. A high percentage of potash in a soil seems capable of making up for a low percentage of lime_, and, conversely, a soil very rich in lime and phosphoric acid may be very fertile notwithstanding a low percent- age of potash. The average annual consumption of potash for raising- crops is 45 pounds per acre, or about .002 per cent. Soda. — This is a less important constituent in soil than ])otash, and unless near the sea coast is present in even smaller quantities. Under the form of common salt, however, its presence is a cause of sterility in the soil when it exceeds .10 per cent, in quantity. Magnesia is found in all fertile soils^ in different proportions, often amounting to a mere trace. In the majority of cases the percentage !6f magnesia is greater than that of the lime, but it does not seem capable of performing, to any appreciable extent the general function of lime in soil improvement. 38 RESOURCES OF DAKOTA. Sulphuric acid and chlorine occur very sparingly in most soils. From .02 to .04 per cent, of the former seems to be adequate to most soils. There does not exist any affinity between the quantities of lime and magnesia contained in soils and those of potash and of phosphoric acid. Nitrogen and Nitrates. — The natural sources of nitrogen in crops are the nitrates and ammonia salts, which are seldom present in large quantities, and should be used on or generated in the soil as rapidly as crops require them. The process of nitrification, whereby inert or unassimilable nitro- gen becomes converted into nitric acid, is thus of great importance to agriculturists. This is due to a minute bactarium present in all soils, whereby the humus and ammonia are oxidized and the nitrogen con- verted into nitric acid. This process does not take place unless the soil is moist and has free access of air, and some base, generally lime, is pres- ent, with which the nitric acid can combine. Nitrification is thus most active in summer, and ceases, apparently, in winter. In carrying on these investigations by the National Department of Ag- riculture, samples of thirty different soils, taken from widely separated areas of the United States, were completely analyzed by the chemist, and three of these sample- were of prairie soils from Dakota. The result of the analysis of the samples from Dakota is given in full below: ANALYSIS OF THREE SAMPLES OP AIR-DRIED DAKOTA SOILS. (By Edgar Richards. Chemist U. S. Department of Agriculture ) Samples. Component parts. Xo. 1. : No. 2. No. 3. Percentage of: Hygroscopic moisture 6.275 7.800 7.700 Insoluble silica V i 53.415 30.555 Hydrated silica [\ 00,335 13.020 21.215 Soluble silica J .400 .460 .485 Sesquioxide of iron Fe 2 3 4.006; 4.608 < 3.204 Aluminia. AU0 3 7.052 0.030 7.382 Phosphoric acid, P,,0 5 112 .112 .224 Lime, CaO " 848 ! .852 3.808 Magnesia, MgO .808 1.535 2.007 Potash, K,0.. .720 .725 .745 Soda, NaoO ' .045 .040 1.550 Sulphuric acid, SO, .120 .077 .163 Chlorine, CI .027 .053 .078 Carbonic acid, CO. 220 .104 2.530 Volatile and organic matter 8.005 6.171 10.175 Total ■ 100.013 100.102 100.971 Nitrogen, N I .324 .170 .414 The analysis leads to the following conclusions : First . The remarkable adaptability of Dakota soils to readily imbibe and retain moisture. Of all the samples analyzed by the chemist only one RESOURCES OF DAKOTA. 39 exceeded in the percentage of hygroscopic moisture the lowest amount obtained from eitherjjf the Dakota soils. Second. That, as regards silica in its soluble state, (and in this way only is it valuable as a source of plant food), the Dakota soils rank third on the list of the thirty samples analyzed, and are, therefore, particularly well adapted to the raising of cereal crops, which possess in a marked degree the capacity for feeding~on silicates. And the same is true of the per- centage shown of hydrated silica, which represents that which is grad- ually available for plant food. Third. It contains the average of 4 per cent, of ferric oxide, valuable, because to its presence is chief!}' due the retention of phosphoric acid, and because it tends to make clay lands easier of tillage. Fourth. In the percentage of alumina or clay in the soil, the samples from Dakota, containing an average of over 8 per cent., are again third on the list. Its presence is valuable as furnishing a supply of potash and be- cause it has the important property of absorbing and retaining phosphoric aoid, ammonia, potash, lime, and other substances necessary for plant food. The chemist declares the light clay soil, containing from G to 10 per cent, of alumina, the best for wheat. Fifth. It shows an abundant supply of phosphoric acid which the chemist says, " in general, even in the most fertile soils, is found in very minute quantities." The percentage of phosphoric acid found in sample No. 3, is exceeded in but one of all the soils analyzed. Sixth. The chemist lays down the rule that the percentage of lime in clay loams should not fall below .250 and in heavy clay soils not below .500. The analysis of the samples from Dakota, shows nearly double the last amount in all three instances, and in the case of sample No. 3 it ranks first on the entire list as regards the percentage of lime. Seventh. It will be observed that the percentage of potash varies only slightly in the Dakota samples and is ample for all time- to come. The chemist remarks that a soil containing .125 per cent, should furnish potash for a century, and that high per cent, of potash makes up for a low per- centage of lime. The Dakota samples show a percentage of potash of .720-, .725-. and .745. respectively. Eighth. The analysis shows that the amount of nitrogen in the Dakota soil is very large, and agrees closely in the three samples and that it is rich enough in this necessary soil constituent for the continued raising of abundant crops. Two of the samples of prairie soils rank in this re- spect, third on the list analyzed. • Ninth. The prairie soils contain a percentage of humus, or organic matter, greater than twenty-live out of the thirty samples analyzed. The smallest percentage of humus obtained from an analysis of the three samples w r as, 6.171 and the greatest 10.175, whilst the famous black soil of the Ural mountains in Russia, contains but five to twelve per cent. In the most fertile of soils of this country, vegetable humus occurs only in small quantities. It is hygroscopic, i. e. greatly increases the water hold- 40 RESOURCES OF DAKOTA. ing^ power of soils arid enables them to withstand prolonged drought, be- sides furnishing^ valuable food supply for the growing plants. To sum. up, we rind that the Territory is covered with a rich dark drift or alluvial loam, from, one to four feet deep, underlayed with a clay sub- soil having the: properties of holding moisture to a wonderful degree, which is given out as needed by the growing crops; that it contains an in- exhaustible supply of the most important soil constituents, as soluble silica, lime, potash, soda, phosphoric acid, nitrogen and vegetable humus, and will produce for a life time abundant crops under favorable climatic conditions, and that the soil of Dakota varies but little in the different localities. It would seem that it contains the proper percentage of plant constituents to give it the peculiar chemical composition requisite for producing cereals the richest in albuminoids and the life sustaining pro- perties, for, by Government analysis, it has also been determined that Da- kota wheat and corn take the first rank as regards the percentage of albuminoids and nitrogen of any grown in the United States. It would further appear that Dakota soil is a mixture of sand and clay in the proper proportions to bring about the ready absorption of the rainfall, and to cause-the soil to be easily pulverized. The clay subsoil, also of the drift formation, is of inexhaustible depth and quite as fertile as the top soil". Through the effect of deep winter freezing and the rising of the moisture in the spring, the rich natural fertilizers of the subsoil are constantly being mixed with the top-soil, replacing those taken by the crops and thus assuring the farmers of Dakota in the possession of a soil, which is as nearly inexhaustible as any on the face of the globe. The fertility of the sub-soil has been practically demonstrated by growing on it alone, the most luxuriant vegetable growth. In addition to the Government analysis referred to, a section of Dakota, soil was some time ago subjected to a chemical analysis by Dr. A. P. ATtken, of Edinburgh, Scotland, anabyst to the Grain Exchange of that city, who pronounced it the most interesting soil he had ever investigated. He! particularly dwells upon the texture being such, as to permit of the rapid using of moisture from beneath, and declares that he demonstrated it by experiment, to be capable of raising water eighteen inches one day, "thus showing" as he says, "its suitability to withstand drought." With regard to. its fertility, he continues, "the amount of salts, soluble in water 4 is naturally greatest in the upper layer of the section submitted to him, but that the very slight diminution in the quantity of soluble salts in the lowest layer from that contained in the middle layer, indicates that even at great depth the soil may be comparitively well supplied with salts, soluble in wafer, and immedietely available for the use of crops." And also, as an Important feature of the soil, the proportion of phosphoric acid, potash and lime actually increases with the depth, so that, as the superficial layer becomes exhausted, its fertaility will be replenished by stores of nourishment from beneath. The editor of the United Slates Med- RESOURCES OF DAKOTA. 41 ical Investigator of Chicago, himself a scientist wJio has given jn.ncli.time and thought to the study of the soils, writes as follows .of. Dakota: "The lands east of the Mississippi have had their saline ingredients washed ont and carried away to the ocean or under ground, jand. are now being tapped at Saginaw and other salt works. Dakota.retains her valua- ble saline soil ingredients, chiefly, I judge, on account of the deep loam, numerous irregular strata of clay, and the level character Df the surface. Some of it is undoubtedly being carried off by the many rivers, and more will be when cultivation becomes general. There is a current theory that the saline ingredients are chiefly due to the periodical prairie fires that have swept over the land, depositing an ash which, being absorbed, •gives to the water its brackish character. That is true to a certain extent, yet I am of the opinion that the fires, like the washings of the water, les- sen rather than increase the amount of these peculiar soda soil ingredi- ents. The saline character is rather duej as we have intimated, to the sediment deposited from decomposed inorganic material in the ages lang syne. '•The soil is evidently a glacial drift deposit, and. like portions of Switzer- land, is filled with vegetable matter many feet deep. There are no dis- tinct layers of either clay, sand or gravel. What the rock deposit beneath is, will be interesting to find out. "The soil will prove inexhaustible, and when the surface is unproductive deep sub-soil plowing will rejuvenate it by bringing' to the surface valua- ble saline soil. The rolling land will therefore prove as valuable as the lower levels, while the low swales can be rendered productive by drain- ing or boring for several feet down . The fact thatpockets df sand, gravel, clay and alluvial deposit are mixed, and that stumps of trees are found thirty feet below the surface, shows that the soil is something wonderful. It will interest students of geology, and those interested in continent formation, to visit this wonderful country. "When we come to study the soil water of Dakota; we shall see that this soil composition is undoubtedly very favorable to absorption and reten- tion of moisture. Sulphuric acid, it is well known to alchemists, absorbs moisture rapidly from the air. An open vial partially filled with sul- phuric acid will soon absorb enough water from the air to overflow the vial. Salt also absorbs moisture from the air. With these facts before him, the agricultural chemist would not be surprised that the soil, rich in the sulphates and containing salts,would absorb and retain such moisture. "The fact that many of the lakes are in the higher regions would seem to indicate that the moisture is largely absorbed from the atmosphere. Soils which attract aerial moisture are found to contain sand, finely di- vided clay, carbonate of lime, and organic matter, all so lightly bound to- gether as to permit of the perfect access of air to a considerable depth. (Griffith's Chemistry of the Four Seasons.) Another thing which may 42 RESOURCES OF DAKOTA. partially account for the moisture is the clouds hang low over a treeless, level country, which greatly favors precipitation. X * XX X X "The lightness and porosity of the freshly upturned soil ofDakotaisa marvel to one who would expect sogginess from the luxuriant growth of grass. This lightness suggests sand and shallowness, but we see that it is a salient feature of rich land. Nature has pursued a conservative course toward Dakota, enabling her to hoard her wealth, and her citizens should bear this ever in mind, so as to increase the treasury of this won- derful country. It will be years yet before this land will need enriching. There is no region that I know of with so generally rich a soil." The adaptability of the soil to readily absorb moisture is observed when one considers the splendid condition of our prairie roads, which are al- ways passa'ble even after the heaviest of rain storms. They are never muddy and heavy, as results during the long rainy season of the Eastern states. Nearly the entire surface of the Territory consists of arable lands, with an easily tilled, rich, and productive soil, such as has been described. No clearing of trees or removing of stumps is necessary. The land lies open, in broad, fertile expanses awaiting the plow and the work of culti- vation. RESOURCES OF DAKOTA. 43 CLIMATE OF DAKOTA. Scarcely anything connected with Dakota is the subject of greater mis- conception than its climate. When one talks of a removal to Minnesota, Michigan, Wisconsin or Iowa, the climate of those prosperous and old settled states is not thought to offer an insurmountable objection; but the very moment Dakota is mentioned, whose boundaries are practically within the same latitudes as the states named,, we are told of long dreaiy win- ters, terrible blizzards, and disastrous cyclones. It is difficult to under- stand in what manner the climate of the Territory.came to be so misrepre- sented to our Eastern neighbors; certainly there never existed greater ignorance than is sometimes displayed, by the remarks of people and the press of the East, on the weather of Dakota. However. each»year peo- ple are hearing more and more about the Territory; they are consulting the maps and weather reports, and the truth is gradually becoming known. They see that Dakota is in the same latitude as many of the most prosperous and well-to-do states of the Union; that man;, of her towns are no father north than the villages of Vermont, New Hampshire, northern Iowa and New York, and that every one of her cities compares favorably, in location, with those in the states of ' Minnesota, Wisconsin and Michigan. Dakota contains millions of acres of land in identically the same latitude as a portion of the great and nourishing state of Iowa, which state forms apart of the eastern boundary of the Territory, and millions of acres in a more southern latitude than any within the state of Minnesota. Even if latitude were the only cause to determine the character of climate. Dakota is as favorably located as many of the states of the Union. But scientific investigation lias demonstrated the fact that latitude is not the one factor that regulates the severity of the winter months. A number of cities located in the same latitude have a difference in their mean temperature for January, of from r2°" to 75° , all brought about by the tempering influences of streams of equatorial warmth, which are dis- tributed through the ocean currents. Great Britain would scarcely be habitable were it not for her proximity to these warm ocean currents. The isothermal line (that is an imaginary line passing through points having the same mean annual temperature), of.40°-50° mean annual tem- perature, passes through the wheat countries of Russia, Austria and France, and. in the United States, runs westward through Harrisburg, 44 RESOURCES OF DAKOTA. Cleveland and. Chicago, turns northward to St. Paul, and passes westward north of the- northern boundary line of Dakota and Montana. The sudden trend, of the. isothermal line northward following the course of the Mis- souri river, marks its meeting with the warm Japan currents known as "Chinook winds/' which, flow from the tropical waters of the Indian ocean, along the costs of Asia and Japan, through the Pacific ocean, and are finally distributed over the territories of Washington, Montana, and Dakota, sensibly tempering the climate of the entire Northwest. The atmosphere is dry and devoid of any humidity during the winter months, and therefore ft never penetrates and chills as does the damp at- mosphere of the Atlantic states. It is a fact borne out by the assertions of all the residents of the Territory, hailing, as they do, from all sections of the United States, that the winters of Dakota are no more severe and cause less suffering and inconvenience, than the winters of the New Eng- land or Western states. The thermometer occasionally registers a very low temperature, and probably this is the cause of so much inexcusable mis- conception in regard to our climate ; but the reader is assured that a tem- perature of 40° below zero, an exceptionally cold day of the winter, has no more terrors for a Dakotaian, than has the " norther " of Texas or the daily snow storms, of New England for the residents of those localities. The winters are cold, it is true, but the air is dry, pure and full of in- vigo ration,; and w r ith every respiration one feels that he is drinking from the mythical spring of perpetual youth. Less snow falls in Dakota during the winter than in the states east and south of us. As a general rule there is scarcety enough snow to make good sleighing. The railroads of the Territory are very much less obstructed from snow than in any other lo- cality of the same latitude. Occasionally, Dakota is visited with unusually severe weather, accompanied by a greater amount of snowfall, as was true during the winter of 1880-7 ; but such extreme visitations are the rare oc- currences that happen even to the most favored sections of the globe. The most disagreeable and uncomfortable days of the winter are not those indicated by the lowest temperature, as our Eastern friends would imagine. It is only when the wind blows strong from the northwest, full of fine par- ticles of snow, that the Dakotaian thinks of housing himself because of the inclemency of the weather. These storms, popularly known as bliz- zards, are quite severe, but fortunately are rare, and are always followed by days brighter and more sunshiny if possible, than those of the stand- ard for this season of the year. The records of the National Weather Bureau prove the assertion that, in the winter months, Dakota enjoys more sunny days, (days when persons and teams are comfortable out of doors), than any of the states of the East. The autumn is a delfghtful season, and is generally prolonged far into December; set cold weather rarely visiting us till after the holidays. The sudden breaking up erf the winters is a very noticeable feature of Dakota weather. There fs none of that intermittent warfare between Boreas and the sun, resulting in a prolonged visitation of rain and wind, alternate RESOURCES OF DAKOTA. 45 freezing and thawing, so common in the Eastern states, and dreaded al- ways as the most disagreeable season of the year. The winter breaks in March, usually, and is followed immediately by the warm, sunny days of summer. Seeding and farm operations generally begin in the latter part of March, or early in April, and are seldom inter- rupted by the return of frost or snow: Occasionally, in the southern por- tion of the Territory, seeding is begun as early as February, and the fall plowing continued as late as December. There is little question but that the cultivation of the soil, the planting of trees, and the improvements of civilization, have already had a marked effect on the climate of Dakota. Some of the oldest settlers insist that, even within their time, these changes have been very decided, and that seeding is now begun a month earlier than formerly. The summer time is characterized by warm days and cool nights. Da- kota has established her claim to many advantages when the question of a home is being considered, and none is more universally admitted than her beautiful evenings and cool, pleasant nights. The day may have been a little too warm to be comfortable ; the winds high and stormy, but at night all is calm and peaceful, and the tired laborer or wear}' invalid never fails of finding rest in the delightful hours of the cool, slumber- giving night season. In reality the pure, exhilarating, healthful climate of Dakota is one of the enchantments by means of which she holds irre- sistibly within her grasp, those who have enjoyed a residence within her boundaries, be it never so short. The visitor, who has once drunk deep draughts of this prairie oxygen, is under the charmer's spell, and can never again content himself to live without the Territory. The story of the prodigal's return was never more truthfully represented than by those of our people who, having earned a competency, attempt to become reconciled to the old home in the East. The effort invariably ends in miserable failure and a return to the delightful climate of Dakota. This fact alone ought to be a sufficient argument to remove any doubts the reader may entertain in regard to our weather. Of cyclones and like disastrous storms, the people of Dakota have no fear. The investigations of the United States Signal Service declare us to be without the cyclone belt. Each year's record tells of death -dealing cyclones, of terrible floods, of forest tires, of drought and of earthquakes in neighboring states, and yet no one thinks of maligning those sections of the Union by oft repeated exaggerations of their misfortunes. But let Dakota be visited by the least of these disasters and there would fol- low such an outpouring of misrepresentation, topped with glaring head- lines, as would move the very world for sympathy. When the truth in regard to Dakota's climate shall become widely known, she will need no louder songs sung in her praise than will then be uttered by her present ignorant detractors. Intelligently investigated and understood, the healthfullness of the climate offers the strongest and weightiest of all in- ducements for settlement in our midst. 46 RESOURCES OF DAKOTA. TABLES OF WEATHER REPORTS. Through the kind co-operation of the Chief Signal Officer, United States Army, nine stations of the United States Signal Service furnish each month to the Commissioner of Immigration, Dakota, a summary of their observa- tions. These stations are located as follows: Locality. Latitude. Longitude. Missouri Vallev : ' " ' ." Yankton 42 45 97 3 Huron 44 21 98 90 Fort Sully 44 30 101 44 Extreme Northwest: Moorhead 46 51 96 50 St. Vincent 41) 00 97 00 FortTotten 47 57 98 57 Bismarck 46 48 103 5s FortBuford 48 30 100 38 Northern Slope: Deadwood 44 28 103 48 In addition to the data obtained from these regular reports this office has had the advantage, in preparing the weather statistics published in this volume, of consulting the most complete and elaborate set of Dakota weather records ever before compiled, covering, as they do, some thirty widely separated stations in the Territory and extending over a period, in some instances, of fifteen years. These valuable weather records were transcribed expressly for this work, under the direction of General Greely, Chief Signal Officer, Washington, from the original reports, filed in the War Department, of the post surgeons, of all the Government posts estab- lished in Dakota since 1872; the reports of the various signal stations main- tained from time to time in the Territory, and the reports of several vol- untary ol >servers. From these official and reliable reports the following weather tables have been prepared with much labor and care. RESOURCES OF DAKOTA. 47 r. to ice S 1) O 00 5 * fl CO CO O / 03 i — . o 3 C5 p. a oj 43 £ . S"e*2t _; D ■3 2 13 a a ,o ~r-^a :j C OJO DO r - - .- S f& D x . s Cj£3 Moqiuaidag ■jsnSriv '&ia.£ — ~ -i- 1 '. — ~S^1 1 x - V * -J: 5 - ~ - s5 :- wmF o saw >c ^ - - mcn oo so A'!K - Nto -f oc m so oe i> cm o : co _ x *> ^oo'(M i> i»"b"odtf) o o h * o'M t^ cc o co h :_,->- l-l- x tC N tC »" IN "1 00 ■ t> l> £§gbfflSi3 ~- M — 1- — X i" t- l~ "lutfV •qo.ib'K A'imwqog iOi-Ii-~ '~ >" >~ S -r 01 00 X ~< ~ - '<"-' ^ "" ' _• _ ^ -, ~ ^ ~; ,-" -^ x oi .- -t >- r - = ;- = x - '- - '- ^^t^ - -r -j " ' i M - - - -- ' -f -t< CO -r — -r ' CO ■ I ,7 L- CC CC SO I- X X [> ' — — so ri ■ i- c PI bi§SS §SSS« SSpi eofn weft -i _ -_ - •- i- u- :: x i- - — X op r-i X ..? _ ..c x SN - "= - l ^ ■_ — z ^, z. — ~> 71 - ^ m - d - x - -: ^ ^1 - - '- - '- x - 1- ~ l ~. '" t ^ M - x rl L - :? :t - -i- .- - 2j - 12 - Lr !_: '? - x ~ toco i-" oco r-' M :t - - -T 9 - ' "t •"' "f a o :^ : ' 'A ^ : : : : : : - r ^ L • : : 2 5 03 . £ : ; :i>-§"' O o5 03 >C > : • : o r """ ^ ^ -5 i. x ^ ^ i. _ - - • 48 RESOURCES OF DAKOTA. From the above table it will be seen that January is the coldest month in the year in Dakota, and July the warmest. The weather is six degrees warmer in February than January and nearly three degrees warmer m December than in January or February. The average temperature of of the three winter months in Dakota, covering a long period of years, is 11.8°. For the spring months the average temperature is 41.1° — or about the mean annual temperature of the Territory. In March the weather is •nearly 12 degrees warmer than the preceding month, April 18 degrees warmer than March, and May 14 degrees warmer than April. The average temperature during the summer time is 69.1°. In June the weather grows warmer by 9 degrees, and in July the maximum temperature of the season is reached, viz. : 71.8°. During August the thermometer begins to fall, and the average temperature of this month is 2 degrees and a fraction below that of July. The average temperature during the fall is 3 degrees higher than during the three months of spring, viz.: 44.1°. In September the thermometer averages 10.8° lower than in August, October 13.1° below September, and November 18° lower than October. The following table, wherein the average state of the weather in Dakota, based on observations covering a period of fifteen years, is compared with the monthly and annual mean temperature of one of the New England and one of the Western states, shows that in no month of the year does the weather average so cold in Dakota as in either Minnesota or New Hampshire : >~> m c3 d c3 c3 p CO PR ft 3 Pi J-5 13 1-3 +3 &i) P < o o O a o s o (V 5 3 o o o 6 o o 6" o o o o o o Dakota 6.8 12.9 24.2 42.5 56.7 65.8 71.8 69.6 58.8 45.7 27.7 15.6 41.5 Minnesota 3.2 6.1 10.2 8.8 20.5 9.6 38.5 20.1 52.8 34.2 63.0 44.3 66.2 46.7 65.8 47.2 56.0 42.6 44.1 30.2 25.5 17.2 11.6 11.3 38.1 New Hampshire 26.5 RESOURCES OF DAKOTA. 40 H 3 o 3(i;ci| ce * o Cy 3 « iOO>OH!000!OQO«iK>0000>>0(Ot»t-«)cOO>OMHH^01«) I t> , M-ir:!OKKMo6«coi* — -r -r -r -r -r -r -f i-O -rco iO -f -c -f -f -f -r -f -r -f 10 -r -f -^r -r 1 ! o 5 - <0 I-H &3 aj j tf 0) P « 1 f_i * < .d pH « W o3 1 ^ ^ 1 S £j H > H 60 fl ^ £ — a - -T- t> o o cm co co u: X' X ' X CN ' HOOi d ec co" [CODiOIOOl d — ' — d » -r — t i" -r cc cr co -* coco CO -* coo OS CM i> d If, x '^ -r ~. — x CO r-i CO t^iOCO i ci i-i cn d ■ — — < — — coco :cm xd CM X i-jd lO CO -CO e-oic- o oii> :3 X O l> i> id a> d lC © X ©» -* d :o — — hHOO r-oo t>aoeo t> oi co m t- 1- o -r ^r -? -r CC l- to o CM d d X ooo_<■« — . &n'jt, .So Gh Eq i=, 22 Et ts. fe fe Et, > SS si ^ o .o 5^ £c1 c - ti * w <» ■ »w P " O . - .<" 3 ^ £ «J & ^ +^.— s. O O 50 RESOURCES OF DAKOTA. ti ^ H i-l pq — a H o > E & < w S w A'-S >■ |fi W — i CO OS rH OS LOOOOiOOOiOtOiOpHOlCOHWC c -> °oi ■'. ri — ' i~ it' ri oi ri — ' 7i i~ — ' rv 71 -~ oi i> -* : =■*-< ~ r^ 71 77 Tt 7! 71 "t 71 71 " " CT :t r— ;,- 71 71 t^ 71 7 m ^ ; ^C»H«0« x c : ^ : : x - ""• "'"■ : H? iHpSJSM§§j|SSSS|S ' ' lQ X 1 ^ !i llisp ;g J. oc cc o J52c>-22iS"^ :^ r; |ss |a |s |ass isaas|8 X CO %k -\ : $% -~a-, !> 00 " ^ [ \~^-' : : .^ M tf ^ ^-r' ■! :-■:, - X 1 T-l .(J -I- ■ r-i.-.- '1 'l 0*>30P1tH Hi7>«;/;i T j CO CO i~ i l V~. "--~:~ j JtH :r-:7X | j ;,-_::: r--r \ j j in j j X os : cq : : to tH os ic « *™ ;;s^ * U oo o : £ ^ : • ^ -,- ,^' • : k- sjsli icisrli i - X 1> X : 7i : : rv i- : : 1 H -:--l r - ~ -■ ii ^ o" '"' ^ ^ ^ C*'^ £j SJcQin -, ** i> o : : x o : : °q6o i :vid i : in cn : : r-( t-h : ; 71 3*ti£ il • 3 i CO oc o j : l- 7i : : °7i :-7 : '■ t>- to : • p i ^ % ; b X o ::::::: I ; : 7i : : : : : l: ::::'*:: s X o ::::::: ■ 71 CO 33 £ £ 7 d A ^Z Z~-i -------- '^ A A c: _ - ^ -'- 52 RESOURCES OF DAKOTA Mean temperature for the month at each locality o -1.0 3.8 3.9 9.3 3.6 4.5 20.9 12.1 5.5 15.9 16.7 17.8 14.8 -5.7 14.7 .r: -t- oc- co oo CM -t ^ cc k cc x o 1 co co d i-5 co co r-5 cm' -* d i-i co co -^ ' co CO CO 1-1 o • : : i I cm i : 3 : : 1 : : CO i>5 CO d 1 CM 1 1 ' CC 8 ___ CO E2 : t- : •'H(Nt> o ; L ~ ; ;^^ • : i : : i i »— ) co : co : d ■ i> j r-5 co ,± 6 .. 1.8 -10.5 4.5 zero . 5.0 -2.4 -6.9 -0.5 : -# join o© : ' : N """' i- : uo : co J -# : . ©■<# d d d t- i co t- : I cm o 5 cm" ^j5 d r-5 1-5 co "© ' : t-h 01 i-i : cm : co o COTji 1 H -th i co cn : Imooiio 1 o j d '• t-5 cn : :i-5codcoli>5 , :hi : : rt i , , :i>coLocouooooocn : cm : I^cicn -t" d co cm' : d | SO CO CO -5.8 -11.1 "-0.7" 7.4 0.7 9 7 zero. :lc jiococTiccioco ;hocoo« ° : d : co — 5 cm cm d r~ •" cm d t>5 d d IrH IHrtHCMHH I (N H H CM co-#cc 00 : : ededdeo j I ^<#lO M j co cm' d 1 ■* ! CM l— i i-H 1 : uO | ■* 113 CO OJ CO : -5 r-5 d d : i : i i i — t \rH-# : : cd d ccici '• '■ i-i r-t cm : : X ~l : cm : : o •* oc -# ° : co : : oc d r-5 cm : : : t-knth io coai cm d^dco CM i-l 1 i-l xohio : : d-* cd cd | | CO Mo ! i|3 : : cn :c : :- : : co t 1 io : : i> r-5 d : ; r-l : d io co co : cm r-- i-O cm Tt< : : io -cri cm j cm r-5 d m d j j — DC : j> lr i o-rd j jt>d j t- t t— 1 1> : i— ! cMr-JT-5 :^j5 1 CMtH ;tH m 1— cm : -f d cdr-i | d d IN i i-t os : : o cm : °©t^ : :dd ' ii : : i y> : r-: as co : co lohh : co d otj5 :d 1 1:1 d I'll- ! : : 1 ' : S i oo Hr CO o 1 o • : o CO : ^ : J> : : 1 co ■ • d " - ' 1 ° ■ ;d 1 II- Ml! 6 h o c u c << Eft S CO CC <£2 E o 3 c£ CD g - i.' - k c: ) — c 3 i IOC - i 'a r M 3 : g a 1 — J - 2S - fl ' S 1 : w : = ^dc 5-c >^5 3 £ > Eargo (Moorhead) Mvan temp. each year for Territory 1 by months; and mean monthly V temp, covering period of years .. ) RESOURCES OF DAKOTA . :c t-. i- .- — x — c 1 x -r. ■— .r. to :t:.:nt 3 co iO lo soiMr.ocr.a oi to o - I Ol t-I CO c to C 51 — CI I — ■ 32 -N 32 : OlM 0)1 §E too-* CO id id OKfrt • L-- £ D O H H n X O CC-fH»C.C0OO id o to i> -j- d ? i m to CO ^dd l-HCN L^ tO °CNCC Oy-J, OS T-i -ti m oo t> X d r-i 00 t£ -p ? 1 - I - I - I I T 1 I 00 O H ■ i S3 d -r I oo a> ic oo 3 £3^ CNOO-^OO cd d ■* id ■O 51 i— ■ oi oi co CO to doi HHlO i~ 51 51 -# CO CO iO 51 t-h 51 d CO CO 51 51 CO d d i> O 53 51 CO d i--i d d Ol tH^ O l-i U5 CO d ■ZTT C ° °8*S ■ 0=to^?^ = : £ => 3 ^ • S 3 S s s =s d ^ <^ .2 -^ o « •" .- r x coco to t> id o id so d d 51 t^ CO CM m o oo d co id 51 to o 5- d oi d d V5 rH K d — ■- oi :o oi XXSlTf 5- ■*■>#-* 00 r-H 01 1 1 CO 01 i-l 51 -^ in: oo oi x i> 00 Ol r->. 51 d d d oi Ol Ol -f 51 d d d ci ~ CC CO 151 o ^ d -. £ v - - = X M fH i« 0) . o:: S^-K^*^ c^tL.-sjtL.SfcGiiE^fcSocui^^aS u-^>^\ fcH = CD t- O >» H H oi r S.2: i- 4 "i CD o g-£ O I 51 RESOURCES OF DAKOTA. H ^ h — o H £ < C a S |zi -<£J fs} .-. H D «t-i 03 « t> X X 3 ^sgja&gs 00 ?M • C ^r C 1 ,t 1 HsHlP^W^l 2_ - $* ,;■; ., « x o : - t ' : ^j ^ y" -j : q • : ^ : : — " — ' : ,~" : ~i = .~ ; ;^r,x,T i- 22 '' 2 ^2,2':;^, .'.: ^ x .", ~. ^ ,2 :r ! i x - ^ -r 1 ^ gj : ■- x x -t — '- — it : ~. : : ts cc ■ : ■ --. x - as : :-i:xr ■- x o ^euio^c^r-V ir: i !o6^ : i Wd- - idd^ 1 « I C M !2S|2S| id |p5 | ; jgSSg \ \ gs X 1 * x 1 n 1 c :^ I22SSS ■ I232S5 ; = ^S ; = ^ x o : ,-' : : ~ -J ,-' ^ : ; ^J : y -/ — ' : : : x .t x -i J '• '• d • • 1 r-5 od < '■ 7T — , ; , — _ '.. v ~'2: :: 2: ~ U 1 ° 12 ; ;dSS ; ;« ; ;3|^ = ff^Jf -, I : u ; ; i - 1 . ; i I s 22 ~'~ ?, ; ;22~i ■ ■ j ?i j ■ ; x ?i?! ; 22 22 'JI ^ j j j e5 i> o ■ ' i '• • • '■ : - • ■ i i : • • ■ :. • : 2^|1 u 1 °~2 SS ^-',2- =-2 2 sSi * 2d: r^ ! -I" 1 i ■! i ; ! 1 i i ■ i« g o ::::::::::::: -" i • IrH i, : l« ; ; r 1 u i : l« : i i -' oo ° :::::::::::■• :>, 7 1880=1 18-0° 1881-2 26.8 1882-3 21.1 1883-4 19.0 1884-5 20.6 1885-6 24.0 1.886-7 1_ 21.8 .9 1872-:; 1873-4 1874-5 1875-6 1876-7 1877-8 1878-9 1879-80 - Mean average for fifteen years The winters of 1874-5 and 1886-7 were the coldest, and the winter of 1877-8 the mildest during the period covered by these observations. TABLE SHOWING DEPTH OF SNOWFALL IX INCHES, IN DAKOTA, During the winter months of 1883-7, as compared with some of the states. (Compiled from the records of the United States Signal Service.) States Dakota. New Yorl Connecticut Michigan Massachusetts Maine New Hampshire Vermont Notwithstanding the fact that the winter of 1886-7 was one of the coldest in the history of the Territory, and was noted for the unusual number of its snow storms, yet the Government records show that less snow fell in Dakota during that season than in many of the states of the East, the snow- fall in some of the states being nearly double that of Dakota. p6 RESOURCES OF DAKOTA. Amid the states of the Union none takes higher rank in wealth and com- mercial importance than New York, Connecticut, Michigan and Massa- chusetts, notwithstanding the occurrence in each, during* the winter months, of occasional heavy snow storms. Dakota, with the richest agri- cultural lands in the world, and undeveloped mineral and manufactur- ing resources of the greatest magnitude, with a more favorable climate than these wealthy and prosperous commonwealths, will continue in the line of rapid growth and develornnent, such as has marked the beginning of her history, until she has reached her rightful position of the firstState in importance in the Northwest. UNMELTED SNOW. Table showing depth of unmelted snow on the ground in Dakota at the end of the Month of March, 1887, as compared with s >me of the states. (Compiled from re ordsof the United States Signal Service.) Dakota Minnesota Iowa Wisconsin. Inches. 1.0 2.0 3.3 3.3 |j Michigan j 4.8 1 1 Pennsylvania ..' | ! Massachusetts . llMaine i Inches. jNewYork.......:.! 12~9 ! New Hampshire! 17.0 j Connecticut 26.0 | Vermont I 35.2 The spring season opens early and without that lingering hesitancy which causes so much misery and discomfort in other places. In proof of this one has only to compare the amount of snow remaining on the ground in Dakota at the end of March, after the severe winter of 1886-7, (the second coldest season in fifteen years), with other localties, as shown by the pre- ceding table. CLEAR, FAIR AND CLOUDY DAYS IN DAKOTA. Table showing the number of clear, fair and cloudy days in Dakota during each month of the year 1886, as shown by observations at the U S. Signal Service Stations in the Territory. January. o February Yankton.... Deadwood. Huron Ft. Sully.... Bismarck... Ft Buford. Ft Tottcn.. 17 211 141 Averagesi j 9|16.5i No No. j No. | 15 8, 14 8 18! 5 14 1 5 J 5.51 fe | a No. No7 12. 4 11! 4 17 M 16 16 14|_ 7.4114.1] 6.5, March. "2 o 8 No No. 10 14 16 April. i \ May. No. 12 8 11 No. 10 No. 18 15 12 7.5,18.2 10.3 ilO. 5111.3 1 III I I No. 8 12 N.».iNo. . 22| ] 16 j I 20 5 181 17! 181 9. 0118. 51 June. No. No. 12 15 18 10 15 10 12 18 7 20 4 17 10 15 2 9 3 3/51 [11. 1115.03.9 RESOURCES OF DAKOTA . CLEAR, FAIR AND CLOUDY DAYS IN DAKOTA — Continued. Stations Yankton... Deadwood. Huron Ft. Sully.. . Bisnmrclc. Ft. Buford Ft. Totten. July. i a i & 1 Q '3 August. ^September. o I m No. No. ! 12 17 17 9 13 1ft | 14 Ifi 24 [l 14 16 ! O I No October. No\ ember.! 1 December. ^ „■ j* 73 1 (_; 'O m Fh o3 . Nol No. No. No >!! U 18 6 9 13 9 t 12 12 6 91 20 2 [\\ 10 12 8| 10| 18 3 11! 4 14 8 11 11 10 .8 114.5 10.5,6.0,110.5 13.6 5.9; 9| 181 4 61 18! 7 7j 20i 4 8.3 17.8 4.9 i i No country in the world can compare with Dakota in the way of clear, bright, sunshiny weather. Three hundred and two days of the year 1886 (and during 1886 we had more disagreeable weather than for many years previous)? were classed by the observers as either fair or clear, leaving but sixty-three days, or an average of only five to each month, which could be called cloudy or stormy. These were distributed throughout the four seasons as follows: winter, 17 cloudy or stormy days; spring, 22; sum- mer, 8; fall, 16. COMPARATIVE TABLE. Table showing the number of clear, fair and cloudy days in Dakota during the year 1886, in comparison with some of the states. (Compiled from the records of the U. S. Signal Office.) Total. No. Dakota Nebraska Rhode Island Kansas Minnesota Illinois Connecticut Wisconsin Iowa Pennsylvania , Massachusetts.... Indiana Maine Ohio Michigan New York New Hampshire. Cloudy Clear Fail- Days. Days. Days. No" ~ No. No. 62.9 126.7 175.4 67.0 124.0 174.0 81.8 122.2 161 .0 88.7 185.0 146.3 97.2 106.0 161.8 102.4 115.4 147.2 108.3 118.8 148.4 109.1 96.8 159.1 118.0 93.3 153.7 118.8 106.2 140.0 128.0 108.0 134.0 128.1 94.5 142.4 129.5 92.3 148.2 180.8 90.4 143.8 135.8 83.1 146.6 153.5 76.1 185.4 163.6 79.2 122.2 505.0 58 RESOURCES OF DAKOTA. | ft o s d 3 : p- a: OQ O © d5 s o 3 OJj X o £ . o > ' p - "3 So >'x x x f : " S o ~ o K it O M ■+ J .rH *- ^ OB »i ^ > ~ S r- P . .2 S 2 x g 9H —-^ P> o .^ c „ <£ _ & x ft M g D X X ~ gj £ ; x > ft I x § | I s 3 &C *ft~ .■ » bi ~ ~S lii g ! 3 1 : = oS= ft.|il|.l" " " £ t> ft X > ft> X p, "H V 05 •= o .5 'O A-SP-d t3 ;_ X ;. ci o o o . . . O - - - : s -. : s = = ::-:ss = = =-=- a) o ft p OC .~3 3 * rt Si g date, Oct 1878. > date. Any. 1877. CO date. o May 1883. > date. o date. o Aug. 1876. to date. to date. i date. > date. ) date. "5 3 +3 C ~ 2 ^ ti °* a? 3 ® OS /»s r^— Z fC J oTj «j 00 oc So <» % «j X ~J 'X 00 3D « OC L ^ i>. x i ' ,-. ^ x Vr -/ x x -X i- X X X X ± X X X » £ — x X X s T_ 'T 23 I—I 1-1 . « ■ 1 T-, > "I _ T— ,-| ■ 1 _, T"l I"! I"! 43 ►--. >-. f?, . . >J ■ ■ ■ >>+= >. r*s ~ > >■ >. J. ■'■*- >■ »»■< >. i '^ - _• >. o ~~.-z ^5 O-s .^i-:-5X --Sl-S>-3>-S ^^^.^X' ---.--: .--- •Xlt[H0 -o[ qoBa 'joj uotie;idtDa.id [BtiuuB o«apj •laqtuaoaa -l.O^ \ U V A rx-\ ■JaqtuaAO^j ■laqoj.iQ •jcaqui a^dag •;sn§ny •Ainf •autif a' * I a II •tl0.i^KJ = -f._ Ai^niqa j| d R "f. c "-. -. I S : © : : : oc : : :< : : 't ^t r- x i~ it :t £^ :t I ^ •• : : £3 :^'0-x :^g • : igJ^ 1 -* RESOURCES OF DAKOTA. 59 Beginning with January, in Dakota, the month of the year when tin moisture is precipitated, there is a slight increase of Snowfall in February, which is nearly doubled in quantity by the rain and snowfall of March. In April the average rainfall is 2.50 inches, or twice the depth of moisture falling in the preceding month. This is increased 30 per cent, in May, the average precipitation of the month being 3.20 inches, while in June, at just the time the rainfall is most needed to benefit the growingferops in this region of late harvests, the maximum precipitation during any single month of the year is reached, averaging 3.04 inches. During the last half of the year the amount of moisture precipitated each month lessens in about the same ratio as it increases during the first half. By seasons we have the following result: In the winter months the total precipitation averages 2.2o inches; in the spring, (3.96 inches; in the'sum- mer, 9.39 inches, and in the fall 3.77 inches. 00 RESOURCES OF DAKOTA. £ - ft H O <1 Ph O h-i '£ : ) 0! 3 Ph Ph" OS Ph till W o « > H u ,3 kn £ i—i C > H c a tn cc o W bo uj fl OJ +s ««! at) H P ^ o o f- « - 3/ -M CJ 3 I> DO GO CM SO CS rH CM CO CM CM tH iO CM rH CM ^aOMOlOOt-HOO^Oi " "OOl^iCi-Ot^O' (MO)MH r-< ,-hCOi— 'CO CUMHJh IMWriCO : co ^ co co o t- CO i- co 10 o O r-l o o i- ! oaaocoo ai a> t- co cm pq-a 5 C£ CO • CO O CO TCJLO-^ CM CO CM CM ctoan iOOWlO CM CM O Ol t* l-r-00^ ' ^P i> ic cm' io I co w 5"cd ©j?S>: *5 > as m - ~ -,5=&^ds^ 5«--5'«i.SS ?^9?=s2° ^^«Sg3?'oSteg«sES'2 Qj ci^5SSagS^|^ jg-o ffi n a) Its >-< bc^-r ri 2) z. hJ as > 2 ferH<*H RESOURCES OF DAKOTA. (il rj f-> >-. %.&+* a 3 o 05 o cS • O lO I- CO «3 t^ lO I> O rf r4 M ffl CO lO O LO iO M C j K t» 7J » O X Tf CoO-*^Lti(»WOCOO«QO'*MCCfflMritOCNO«^OtO(Nr-CN ElS s " i-i :>i co cm cm cm -r co co co i-i -t< •<* -ct< cm -t -# cq co cm cm cm c\ i-h oi co -^ r-t cm 1882 ; 1883 1884 ! 1885 ; 1886 | 1887 3 : : •:>— iiocm: :co: : : : o : • : : : : t- : : : co : i> lo : r : cm : lo r-5 • * i r-i • c4 o CO oi ■ : o : : co -* rH • :co : •>- : : io cm : : :^t< : co lo co : cm gj cm i-h 3 : i— : : t- -* o • : i-o : o : : io to ; • : to : oo t^ cm ; co co oj io "* -1-1 • ;HHH : '; i-H " O • : rH CM : j • r-i • o cm cm 'omhin CM • : ■<* : o cm cm -^> : :o : th : ioio io : oj : o o t~ :coHcef> 3 : co : -* oj o cm : : oi : co ; ; -rf l- ; os : i> : i> i> ih ,coo^« • i-i ; m o h n • • io • o • • i-i r-i -co • r-5 ■ •CM -ciNOrl • O CM • CO -sfi ■ rH 1-4 -r-i ; CO '• O i-i r-i ifflHOH CO CN • : o "# io io oj co : co io : r- o ■ o o • : -1-1050005 •' • cj -0 00 oj 3 : 1- co co 1- lo co : co -^ : 00 • 00 1> • • -loioiot- ■ • o» i> 00 »o • r-1 O CM r-i O O : Tji -* • Oi •& • i-< T* ; ;NCMH • ; CO 00 O CO CO CO • :ooioor-io :-wo :r~oi>o : : : : o oj — o : : : >o -r cm 3 :cooc:^oo : lo io : co r- h >o : : : : cm ■* co co : : : cm o co 1-1 :CNHHBnl> "CM-* ' CO CM CO CM j j * j CM CM r-i rH j j | LO CM U3 o o CO rH CO CO o t- 00 00 l> 00 t- 00 ! S 00 IO t> 00 T CO § CO c _o CO • : o ! o i> o o : cm : looco^ia '• '■ :m^oio : .* : oo : o 3 : to :nNOb : oj : : co ■* o cr. o : : : >o co ov o : : : oo : oo :co :-*cMi-ico :co . : « i- o co -i : : : cm cm cm cm • j • oj -cm . . r-1 ... .... fl ■ : o -a< .co ; ; :rfiCJo.cM : : .-io^coco : : :o : : : i-i : : cm -*i ci -co • • : co o r^ o • • • co cm r-i -^ : : • -* : • CO CO • : o "• • i^ co co : -rf : ■ 'uoo^o : : : o lo o o : • : lo : - : C : CO ; : o i.O O ; O • : : CO co io ■* ; ; ; LO CO r~ CO ; ; : CO ; ; : co : : co >o lo : co • • • uo cm ih co • • • tji co •* co • • • cm • • OJ OJ CO • :o : tiooo : : :co :ococmooo : : o to i> oo : •' : ■># : 1 S -CO ; ;r-itOCO ; : :oj : OO rtHCl OJ ■* ; ; O CO -* CO ; ; ; O : • " ; r- : : co oi t- • • ' r-i • cm cm i cm i -* ^ • • cm o co cm • • • rji j : iro o CO • co co : iioo •' o •' : co '■ : :iomuo : r- : ^ct* cm i-i : : : o •' • SOCO ; .rH lO ;cO • ; rH ; ; ; t- rH t»i ;OJ .l>0-cfi ; ; . ^ ; ; -r, CN^i • •-*-* -Tt< • -co • ; i-cticcni -r-i • rji -* ■<* • • --r : • - • o co : : -h< o •' o : '-co : : : lo o >o : 10 : o i> cm : co i lo ■ : S CM .V : j 1-- O ; O ; ; ?l ; : : lOI--1- ; r-i ; iji CO OJ : ^ ;n . ; "~ o ■* : : io Tji -co • • © • • ■ o cm co • ni ■ ■* ih co -r-i • cc ■ ■ CO CO CO • i— o : : o oj : o • • : : '■ '• i^~ o- r-i : l^- : co cm i^ : o • ■ -rf • • hHCJ ; ;^J • ; ;;:;;;:::;:::: cm • ::•• 1 co ••■• co • • o d j : j : ' : • I 1 • • 1 • •» • : : • • : 2° ■ - ' 1 • : : : • • ^ : : : . ;::::: oq ■ • ■ • oo' Ft. Abercrombie Ft. A Lincoln Alexandria Ft. Bennett Bismarck Ft Buford Firestoel , Ft. Hale Huron Ft. Meade Olivet .. Ft. Randall Ft. Rice Richardton Ft. Sisseton Ft. Sullv : ' o : . S . -S a I '■ : « : ■ i ;?( - a- S£ i s -1 CC 3

> C ■ IS ! si 62 RESOURCES OF DAKOTA .5 ■c'5 " "* -° : 5 d JIB •S52w:22SS2^^« r S3c iSS22^ - *s X 30 9 >''" * ^ * II MI2 IS [2 Jgijg : — L - ?, ; "t X * |2 :^ri5^ j p :-- : 122 IS 12 IS 2 2 iSSSS ^ -* X X -- • •' -m i- — i — r~ so : i- : a i ~ a • — S '■ '■ '■ ~ : oo •—! ~ "- 1 ^ '■ ■ t£ ■ - ci O 3-d - 05 if ' S ►,0) I! 52 iD — 3 ^ i £ * X RESOURCES OF DAKOTA. 63 HCCIMM r-i i 1> 00 : • 1 jOiOO j : co : OJ :f5 S3 § = N CO : '. : I -r I " C j :"* 1 1 : 1^ i co -t A CO ■ o : ----- i- I ; © : oo • : o ■<* • o : -r ci : ■ CO cc --c -r- 00 : r-i : ;h6« : H • co • ■ co 3 ■ c 1 ; ON : CN r-l rHOCNL'5 oi i (M : i- - « ir : ■' CN : ci • • o oo : : : ~fi : ^, ca ic : t^- 1^ o — j »c OC « : cc : it -r co -r : : "3 : ■-" : : r- oo : : : r> : t- co co ■ c. ~. cc co s . CO •ei ii-5eieor- : i"* : r-i : : co co : • • co '• on d on • -<# r-i o4 co cc . — ; Ci <-i : : o : : : cn : : d : oi : r- irr : \\C co p cj cc s 9 : x : t> cc x it : : r-i i : co : ifl _ CI CO 1-1 . : ^. :o(NO! on ~ cn ■' ON O • oo :^ c: : ■ i X -CO -rH : : cn co -. t^ CO X d : O'M^K ~ x ■ 00 71 - 00 ct : r- X ; : ; — ; cn oc : ■ cc cc r. it ^. s ;' ON CO T-i H t-i r-5 • CO ifl ■ CN d •«•*•* : : : H : '^ T ~ ": '• oi cc ~ -r oi CN CO io-ooJHLOTH : x x : (ft o «> o o : : • cn -rt"M co : -'r-,0 COCN 1 CO 3 : to i> on co cn oc : CV X : o co as to ;o : : • — co t— . o , ;?i- CC. 1 -_-. 00 . -# oo on -# on -# • r i ic • co t« o-i t-^ r-i • 1 : I> -rji CN r-i : : 00 r-i ON -r^ CO : ~ : io oo(M co : - : m on oc m X X : o o o o .t : : : to r-i co o : — : t^ oi , 80 1881 .- CN lC : l-t -r cc — co : • ; 00 O 00 rr ; ; :^ ■- 1 x :,_; :^^^_ i CN :- ■ rA CN rH O r-i ■ • • 01 iC r- : : ; o oc St -■ : : . cc : ; it GO rH • o • : oi -t r-i c : | r-i H CN -sji 00 : ■ : co c -i oi ■ : : cc j j oi : it : : I- CO CN i- : :»omh i - : oo in re i : : -r i : .. 1 1^ — : to • : cn irjcc : :or^icci : : : ■- '■ : in S ; it • ; rH ; O co ; o\ cn >-o x n : lo ~- — x ;::--:: i> s j® : i ~" ; 7 ' CO • O lii •<& t— CN ■ I co d i> cn ; i- ; ; - ic -r : 'NO i -r : cc co t- ~ co O ; OCI ■* rr CO : oi r- ~ . -" : : : i-i : ■ — -r -r : : io oo : : i^ rrl to r-l : : : cc . ; CC CC 1 *r oi : ■ cn d ? CN : r-i CO r-i -f CO ': ^ d«id : 1 H : i oi co : : : cn io os : CN : M : o •' — : : l> r-i •* ; : -r 5 ■ ic -t : : ; : - : i^ :io ihcn to ice : : C; = : : : : : : ■— • t~ u; : x ; rr lQ CO : i> : lo : : cc OC ~ d ' ■ r-i r-i | o • • • '• : • r-i o d : d ! CN ~ — • oi ' it •' • __• ■ -. . - : : : -r : : : : : — — ci : r- : r2 ^ <§ : co : -r : i 1 co ; i> £ on — : ; -on : : : • : -r i- oi : Cfi • r " : cc : ; 1 i— i | CO rio • • ' c • • • '■ • r-i cn d : ° : - cc cr r- Ct j r- co _• 1 ! : ! : • 1 : : : • i^ : : CC x ; : : :g I ! 1 3 CO : : : I 1-1 : : 1-1 : : : I th : : 1 ^ CN x : :::::: l co ! : : : : : -rji e ■sp : CO _IL_ ~^ : ::::■•! -o^ : : : : • i.erc ..... : +i fn ■? pH f^ S < 64 RESOURCES OF DAKOTA. Mean rainfall for month for each locality. in .2.18 2.14 3.20 2.21 2.60 1 . 62 O3OJOIr-^O)i#0^-^CM©C0CC — © ^. CO © CO --rf © CO © t-H i.O t- oioioJcocMT-icocooico^ico^- 2.37 2.91 2.13 2.87 3.87 4.12 2.58 3.05 t-CN CO^ © © oi Io 3 : : : :mh(n : '■ '■ '• '■ '• '■ co : ■ : : : : o« *o : ; : © lie w : : co © cm : : : : : : . : © : : : : : ■- eo ; : ; -^ :•* l- ••THcoco:::::::rH:i:::;coc'i;::-*:T--i|i x i CO 1 5 §§ 1 OC' i CO i ^ • : o : : >c t- tj< i :oi : © : : ic >o : o :co : .-< © : ioohn 3 : © : ;^cooo ; : © : io : : oi c i it : oi ; *<# ^ : :w*cm m rt ! r-5 : ;hoh ': |io : T-i : :o^r ■ r-n ■ rH j r-i rH • • CM lO SO ' © 2 1 • io : i> ?i a m : : © : oj : : © r- : o : © :ont- : t-i — . o r- 1 r-- i a : io ; oc to c cs : : co : oj : : oi th ; oo : p- ; io © oo : ^* o< n ■* © j 1-1 j : :so :© : '• '• as :© :io :oioi : :hhoi> 1 in I © : : t-i : co : : : so : ■<* : ■* : t- »> : :-t©©i-i co co • : T-i ■ 01 • : ! 01 : © : co J © co : • © oi ■* © co | oi : oo t- • oo o ' co © •' • • oi : oo © : : -^ io © © CO .GC1> • r- ■ CO -CC© • • -oi •©-* : 100 00 JH ^4 • oi i-i • © oi _• oi >-i : : ■ oi • oo yh ■ : i-< cm © co 5! • : =5 3 ■ O ' rt -oi hinool- -o-i^ch :tt©tt<©© : ; : -^t-i©t-i : :©lo©io • • :©cm©tf : • :t^ :© . CM © r-lLO l>CO lC © © iC X • • CO HLO Oi • \ \lr~ \ 00 • oioii-H© 'oico '>- ao co cc co ■ • .c^aicNoo : ; : © : : 1-1 • lo • :^"mm io : co it. io -* co ; ■ • ia t-i ■<■: oo ■ • : co : • 1875 • 1876 1877 , 1878 1879 • : oo ! : © oo © .^f 1 ; • © © cm = © : • • © © t-i © ■ : : co : : a oo ■ 'Crr* • io • • ^p t- » © © • . i— o •<*< co • ; : © : : jo j :cioH : © : j n t-h oi © r-i : : j © r-i oi co : • ■ rH ; • 2 • ■ © • : c> o t-h • ^ I vt. : o th t-h o o : : o '■ © © i ; • ■* • : 1 ■* j S CO • 1> © © . • . -f . O n © I"- TK ; ; l> • 00 t> . ■ . ■>* • -jt- | C ; ;NHffi • ■ j r-i j r-i r-i CO O CO • -ti! : © © : ; ; © : • J tH •©© • . lO © • • ■ ■ - •' © r-l T-I © © -CO • r-* -tF © •' • © •' IcO CCOCM • CO© • . • -(NCClCMuO •Ti -©00© • • r-t ■ • •-• ""'©i-l • -O© T-HcN©CNC>i ■© : i— © # ■ • -©Tj 00 • CO CO • • '■ © : • • : • • '. -CM © © 'CO .©!--*< • tJ< - LO ■ • 1 t- S CO CM . • • CN : • • • . . © "» © • l— ■ i-l LO CO -CO . © • • <-~ "^ ■* n • • -CM 1 '• • CO t-I © ■ OI -CO © © -CO • T(< • • (N • s : :::::::; oo '. '. . ..... . CO • • "oi ■ ' i •© i : oo : : '■ '■ "oi • • 00 ! t- 1 oi i CN CO s a "; •' : co • ■ rH : '• \ CO i : : •» 1 CD p XT j j : . ■Dm j; a> • co : • • : i> ■ • : • : ■ . be • • • ;.:;«<:.• • ; ' • ° : : • ^ ' ' : S ® s ■sic-5 c -,* oc^i ^ ci>* &. ^^ n > p : o : — oj CD C 1 : 1^ A o '. 9s '■<- / ^ — i "Sec COCOCC,}- • ■ < : ? : |i • ■ :1 o o GO'S) Io ^ OJO r_ 3-d i CD - a - a 3^ 1 5S KESOURCES OF DAKOTA. 2 o o to (NOOCOiOHOI OHrtrlOl ) CO lO CO Tjt < ICNOCMCai-icSTHr-irHrHrHOr-ieNi' 1 Oi t> O I CO CM O r-t o :-^ ooo ; cd co in Oi oooo ■ o * '^2 DO 1>OCO oh'6 O-HlO r- CO o© t-co din 53^ 2' : r-l CO :doi : oioo ; LC 1^ (N •oho O r-c i-l tH© I-^T-IO it-H(N d r-H id d : t> co t- :i>iho • t-i d co OlCOrli iHoidd- CO 00 O CO ooic* CO i— CN OJ CCOr-lCO eoddd lO 00 CN ddoin coco doi COOOOCM d dd T-i *1 IcO i -d S (3) ■II 3 r"' G .«8 J3 +» s3 6SS S > H w«5 RESOURCES OF DAKOTA. From the above table we find that the total rainfall in Dakota for the five months beginning with April and ending with August, for sixteen years from and including 1872, has been as follows: 1872. 1873. 1874. 1875. 1876. 1877. .14.69 inches. .13.20 .12.63 .13.89 .13.27 .14.74 1878 17.72 1879 15.85 1880 16.21 inches. 1881 13.78 1882 15.47 1883 14.21 1884 15.97 1885 15.90 1886 12.57 1887 15.01 It is instructive to note the gradual but certain increase in the quantity of rainfall throughout the Territory — the undoubted result of the tilling of the soil, the planting of trees, the building of railroads, and other changes brought about by the settlement of the country. The average rainfall during the growing season in Dakota (April to August inclusive), for sixteen years, from 1872 to 1887, has been 14.70 inches. The rainfall covering this period of each year for the first five years from 1871 in every instance fell below the average of 14.70 inches, and for the eleven seasons since 1876 — the date when active settlement of the Territory really began — the quan- tity of rainfall has constantly exceeded this average, with but three ex- ceptions. Dividing this record of six months' rainfall into periods of eight years, we have the following result : The rainfall (five months of the year) from 1872 to 1879, inclusive, aver- aged 14.50 inches. The rainfall (five months of the year) from 1880 to 1887, inclusive, aver- aged 14.89 inches. The quantity of rainfall during the last eight years of the period ex- ceeded that of the first half by a yearly average of 0.39 of an inch. A study of the records of Dakota's weather verifies the assertion made by scientists that the breaking up of the prairies, the growing of forests and the settlement of a country not only modify its climate, but lead to a certain and constant increase in the annual rainfall. RESOURCES OF DAKOTA. 67 HEALTHFULNESS OF THE CLIMATE. Dakota's climate, although the thermometer during tiie winter months sometimes registers considerable coldness, is dry, pure, healthful and in- vigorating, and possesses all the good qualities of the climate of Colorado, without the light, highly raritied air of a mountainous altitude, which is so dangerous to those who have long suffered from lung troubles. The climate, the year around, is especially favorable to pulmonary, bronchial and malarial diseases, and is a builder-up of physical and mental strength and not a detractor from it. as is true of the wet, damp and changeable weather of other localities, and the poisoned atmosphere of all densely populated cities. The invalid, harassed by the murky, heavy atmosphere of the East and sallow from the effects of his daily potations of quinine, experiences an immediate relief with the first deep, long breath of this prairie oxygen. Many settlers who came to Dakota as confirmed invalids now rejoice in the possession of renewed health, as' well as in the owner- ship of comfortable homes amid pleasant surroundings. The number of deaths in the Territory during the census year of 1885, was 2,511, or 6.01 to every 1,000 inhabitants, or 1 in'every 166 of the popula- tion. The following table of the death rate of different localities, compiled from the United States census report of 1880, is certainly a pretty strong argument in favor of Dakota as a health resort: TABLE OF MORTALITY STATISTICS. ...lin 86 Norway Denmark Sweden Great Britain .... Switzerland Holland 1 in 56 ....lin 84 1 in 46 ...1 in 82 lin 50 ...lin 67 1 in 46 ....lin 64 lin 41 All of the United States.. ...lin 66 lin 37 Dakota, (Census of 1885) 1 in 166 The death rate of Sioux Falls last year, which might be taken as a fair sample of other Dakota cities, was 4| to each 1,000 inhabitants; while the average death rate of the leading cities of the country in 1880, according to the census, was 20 to each 1,000. 68 RESOURCES OF DAKOTA. A well known scientific authority, Dr. T. C. Duncan, of Chicago, who visited Dakota for the purpose of making a thorough study of the climate, soil, water, etc., has embodied his views in pamphlet form, and among other things says: " Every country, territory and town has a medical side, and none is more interesting than Dakota. The location, soil, ingredients, water pe- culiarities and rare atmosphere, no doubt, account to a certain extent for its invigorating climate. Besides being rich in agricultural promise, it is des- tined to be a health resort. " The effects of the water upon the health brings me to look at the medi- cal side of the water question: "The person who drinks the well water of Dakota should not be troubled with biliousness, at least not until the soda is replaced by potash, which may take place after long cultivation. "Those who drink water from the Dakota river should not complain of kidney trouble. " The action of magnesia on the bowels is well known. None need buy purgative pills when alkaline water can be drank freely. The sick may take it with decided beneficial results. There are some noted min- eral waters, (i. e. Seidlitz in Germany, Epsom in England, etc.,) in which sulphate Of magnesia, (Epsom salt,) is the leading ingredient. Sulphate of soda, (Glauber's salt,) is a great remedy with many people in this coun- try and Germany. It relieves plethora and constipation. The fat people should visit Dakota and drink bitter well water. Many would, however, prefer the water sent to them. It is the anti-fat. The action of the river water upon the digestive organs will be beneficial. There is nothing in these waters that is deleterious to the health, unless used to excess. "Newcomers should use the alkaline water sparingly, or diarrhcea, loss of appetite, headache and general malaise will follow. People who use the river water will eat well and sleep well. "It is natural for people to look at every country from the standpoint most familiar to the individual, consequently the healthfulness of Dakota was uppermost in my mind as the train rushed on through the wonderful country, rich in ozone and health giving air. ' ' As we passed town after town, I could not help noticing the sanitary surroundings to see whether any settler had violated the health maxim: 'Locate dwellings to the windward of standing water.' Many an early settler's family has suffered years of ill health from a violation of this simple rule. " The flats along the east bank of the Mississippi have always been noto- riously unhealthy. The explanation is easy. Stagnant water generates gases that are unhealthy. Malarial emanations can arise from the large upland ponds that we pass in Dakota, but they can all be easily drained if necessary, so that if any case of chills and fever occurs in Dakota the people themselves will be to blame for it. I have not heard of a case as yet. "I could never quite comprehend why the Northwest competed with RESOURCES OF DAKOTA. 69 California as a health resort, particularly for consumptives, but I now un- derstand it. In several points they are similar, with the exception that the heavy fogs of the California coast are not found here. "First. The nights of both are cool, ensuring sound, invigorating sleep. So marked is this that I shall recommend some of my wakeful, brain- weary patients, business men of Chicago to visit Dakota. "Second. Both have a breeze springing up about ten o'clock in the fore- noon and subsiding toward night. The only difference is that the Dakota breeze is dry air, while the California one is moist, which toward evening becomes chilly — a very disagreeable feature for the feeble. " Third. Both have dust with the wind, but this, although disagreeable, is not a marked objection to the medical man who recognizes the curative power of the dry earth treatment. 'Let children play in the dirt and they will be healthy,' is an old adage. Here the dirt plays with the children, consequently they ought to be healthy. The children here are models of health. This is the land for vigorous, healthy children. " Dakota may yet be as famous for seekers after health as it now is for agricultural interest. I would advise those who would be benefited by a change of climate to visit Dakota. " Before we study the peculiarities of Dakota from a health point of view we will notice the essential requirements of a health resort. It must en- sure first, diversion of mind; second, deep respiration, and third, good digestion. " First. Diversion of mind stands at the front of all the requirements. To one familiar with low land, a visit to the mountains of Colorado, for exam- ple, is a wonderful diversion. It sooths and quiets. There is a majestic awe that steals over the mind. At the same time there is a stimulation that often prompts to over exertion, which may do great injury to the fee- ble. The broad expanse of water, lake or ocean, has a similar effect upon the mind with perhaps a still more soothing effect. The same result is produced by an ocean of prairie. To the citizens of a large city, a trip to the country anywhere is a good diversion. This is an advantage of a sub- urban residence, and a summer visit to some picturesque spot. The healthy diversion of a residence in a great city is familiar to you all. The large cities for health resorts, where mental diversion is the chief require- ment, will yet attract attention more and more. "Second. Deep respiration is a most essential requirement of any health resort. The citizen finds that the rarer air of the country forces its way into all the air cells of his lungs. Those who visit the mountains complain that they cannot get air enough. The air is so rare that they must breathe deeply. The same effect is produced on the ocean, for the reason that there is so much ozone in the atmosphere. The same is true of prairie air. A visit to pine forests, or where luxuriant vegetation absorbs the carbonic acid, has the same effect. The good effect of a trip to the South, especially in winter, with the agreeable diversion from snow to green foliage, is well known. The cool, crisp air of winter, although loaded with 70 RESOURCES OF DAKOTA. ozone and so invigorating to those robust and able to ' drink it in,' yet to the feeble it seems to produce a spasm of the bronchi that interferes with respiration. Diseased and sensitive lungs intuitively keep to the house, or hie away to a mild climate. But this should not be too warm nor supersaturated with moisture, or deep, healthy respiration will be impos- sible. The effect of deep respiration upon the heart and circulation should not be overlooked. If the heart is overtaxed, unfavorable reaction is sure to follow. " Third. Good digestion must be obtained at any good health resort. Where a person eats well and sleeps well, health and vigor come with rapid pace. Passive exercise, like riding m a car in almost any direction, will awaken the appetite of any one. A trip to the mountains usually makes one ' hungry as a bear.' A sea voyage stimulates an appe- tite for sea-biscuits of ten-penny nail consistence, while a ride over the prairies gives an appetite 'like a mowing machine,' as a facetious friend expressed it. " With the mind diverted, and the whole system stimulated by deep respi- ration, the tissues are cleared out, rapid oxidation takes place and ample digestion cares for the body, giving renewed vigor and health. It is as- tonishing the amount of food that can be encompassed at railroad eating houses with only 'twenty minutes for refreshments,' and digested, too, when one is being constantly exercised in a Pullman palace car. Assimi- lation is greatly increased under those circumstances. Good food must be secured at any good health resort ; substantial, palatable food must be obtained. "There are other elements that enter into the requirements of a health resort. One of them is good water. Water, like air, is a form of food. Water aids digestion, assimilation and excretion. " Latitude, as well as altitude, has a direct bearing on the value of a health resort. "The inhabitants at or about a health resort, must be taken into account. Disagreeable and dangerous people can mar and destroy a health resort. Some portions of the Southwest, while excellent locations for the sick, are not yet available for these reasons. "Whether Dakota answers the requirements of a health resort can be gleaned from its characteristics. "It is a vast plateau reached from Chicago after passing up through hill and dale, over rivers and picturesque lakes. As far as the eye can reach for miles and miles, green, waving grass or grain is seen below, and a clear, blue sky above. The effect upon the mind is most soothing. Dakota is so situated that there are constant breezes coming up the rivers, and over the broad expanse of prairie. These increase with the evaporating heavy dews, and wax and wane with the sun, as in California. The lakes and moisture are on the high ground, so that the air is not so dry as in Colo- rado, therefore there is a large amount of ozone always present. The river and surface water is a mild alkaline water. The chief ingredient is mag- RESOURCES OF DAKOTA. 71 nesia. The soil is loaded with saline ingredients which increase the nitro- genous elements of the food, rendering Dakota products very healthful and appetizing. The people of Dakota are vigorous, intelligent, enter- prising and remarkably hospitable. "These are features that, in the opinion of many medical men, will yet make Dakota a famous health resort. "The class of cases that will be especially benefited will readily occur to you. "For consumptives and those suffering with diseases of the lungs, in general, it will yet rival Colorado or California, especially for the first stage of lung troubles. The tax upon the circulation will not be so great as in higher altitudes. Advanced cases had better go South, especially in winter. "The absence of low marshes and malaria make it desirable for those troubled with bilious disorders. " For diseases of the kidney and bladder, the water of Dakota is espe- cially valuable, rivaling that of any noted waters. " For dyspeptics, especially, the climate, water and cereal products of Dakota will yet have a great reputation. " For agreeable,- mental diversion there is no better, safer resort. City business men should take a few weeks' vacation in Dakota, especially in the spring and fall. The mental diversion and physical energy recovered would amply repay them. Young ladies in the East, suffering from neu- rasthenia and ennui, would get health by a short residence in Dakota — as well as a husband, perhaps, and a slice of Government land. "The whole country is filling up rapidly with very intelligent people. In the many towns springing up are excellent openings for young men, with a little money. Money is in great demand. The enterprising railroads that are assisting amazingly to develop this country, will furnish maps and particulars as to special points. Physicians who have visited Dakota agree that the trip is a delightful one. "Dakota is destined, physically, as it is commercially, to wield an im- mense influence in this Nation. It can invite the dyspeptic, hollow- chested young men from the East and expand and develop them into vigorous manhood. The sanitary features of this country should be as widely known as are its agricultural advantages." RESOURCES OF DAKOTA. RIVERS AND LAKES. It is estimated that Dakota has 1,400 square miles of water surface. The principal streams are the Missouri, James or " Jim," Big Sioux, Ver- million, Red, White, Bad, Cheyenne, Moreau, Grand, Cannon Ball, Heart, Sheyenne, Mouse, Little Missouri, and Maple rivers. A great number of lakes are scattered throughout the Territory, nota- bly in the counties of Brookings, Kingsbury, Hamlin, Codington, Wal- worth, Brown, Day, Roberts, Emmons, Logan, Barnes, Stutsman, Kidder, Burleigh, Turner, Benson, Ramsey, Nelson, Foster, Griggs, Deuel, Clark, Charles Mix, Brule, Lake, and Aurora. The Turtle Mountain country, in the counties of Bottineau and Rolette, is full of small lakes and ponds, as is also the wide belt of low hills, the Plateau du Coteau du Missouri, ex- tending diagonally from the northwest to the southeast corners of the Territory. Big Stone lake and Lake Traverse are bodies of water about twenty-five miles long and one or two miles in breadth, forming a portion of the bound- ary line separating Grant and Roberts counties, Dakota, from Minnesota. Devils Lake or Spirit lake of the Indians, situated in Ramsey and Benson counties, is about fifty miles long, with a breadth ranging from a few rods to several miles, and is much the largest lake in the Territory. It covers about 100 square miles of surface and has a shore line of more than 250 miles. The waters of the lake are strongly saline, with a dark green color, resembling that of the ocean. It has no outlet and is surrounded by nar- row belts of heavy, native timber. The lake is the breeding place of myriads of gulls, geese, ducks, snipe, curlew, brant and swan, and is a paradise for sportsmen. It varies in depth from a few feet to more than a hundred, and is elevated some 1,200 feet above the sea. The Missouri river, varying in width from one-fourth of a mile to two miles, is the most important of all the streams of the Territory. It flows in a general southeastern direction, through a course, counting its wind- ings, of fully 1,000 miles within the boundaries of Dakota, dividing the Territory into two nearly equal divisions. Frequent analysis has proved the water in this stream to be the purest river water in the world, al- though no one would imagine this to be true, looking at the 'turgid, muddy, yellow surface of the stream— caused by the great amount of sand* and sediment held in solution. BES0UKCE3 OF DAKOTA. 73 The Missouri is navigable for steamers of several hundred tons burden, eight months of the year; the boats ascending as high as Fort Benton, in Montana, 3,000 miles from where it discharges into the Mississippi, and 4,000 from the Gulf of Mexico. .This river is of the greatest value to the people of Dakota, as a line of transportation, and must ever remain so. No matter how many railroads may be built in the Territory, the river will always serve that great purpose of a regulator of high tariff. By means of the Missouri river every bushel of wheat raised in Dakota could be transported entirely by water to any sea-port of the globe. Tha following account of the early attempts to navigate the upper Mis- souri, from the annual report of the chief of engineers of the United States army, 1883, is of interest: " Up to 1830, the American fur company still clung to their keel or Mack- inac boats, and dragged them by human labor from St. Louis, Missouri, to the mouth of the Yellowstone, in Dakota. In that year, Pierre Choteau and the other members of the company determined to- try a steamboat. The boat was built at Pittsburg, Pa., and in the spring of 1831, left that port for St. Louis. It was called the ' Yellowstone ' and drew three feet eight inches light, five feet loaded. "Succeeded in reaching Fort Pierre, (Stanley county, Dakota), in 1831, but low water prevented further progress, and it returned to St. Louis. In 1832 it succeeded in reaching the mouth of the Yellowstone. This suc- cess led to the building of another boat at Pittsburg, called the ' Assina- boine.' This boat made its first trip in 1833, ascending as high as the mouth of the Yellowstone and returned safely to St. Louis. It repeated the trip in 1834 and 1835. In the latter year, after discharging its cargo at the mouth of the Yellowstone, an experimental trip was made higher up the river, reaching the mouth of the Poplar, in Montana; here it was caught by the falling water and compelled to pass the winter. "The next season, on its way to St. Louis, it was destroyed by fire, in the vicinity of the mouth of the Heart river, opposite the present site of the city of Bismarck. "The American fur company subsequently owned a considerable num- ber of steamboats, and every year saw one or more ascend to the mouth of the Yellowstone. Several attempts were made to push still higher up the river, but with indifferent success as only the ' El Paso ' succeeded in passing the mouth of the Milk river, Montana, and that only a few miles. Mackinac, or keel boats, therefore, continued to be used on the Yellowstone and the Missouri rivers in Montana; but, in 1859, a more determined effort was made. The 'Chippewa' had been built for the company with special reference to the difficulties to be surmounted above the Yellowstone. It had a stern wneel, being the first of that description ever employed on the upper Missouri. The 'Chippewa' left St. Louis in the spring of 1859. It was considered doubtful whether it would be able to pass the shoals above the mouth of the Judith, and a large Mackinac was towed behind to lighten it by unloading the freight, destined for Ft. Benton, Montana. 74 RESOURCES OF DAKOTA. This was done just above'^the mouth of the Judith; the 'Chippewa' passed on and reached a point a few miles beiow Ft. Benton on the 17th of June. Here the]voyage*ended, and, rejoiced at having achieved a suc- cess so decided, Mr. Choteau started the boat for St. Louis. The following year the 'Chippewa' ascended to Ft. Benton, accompanied by the 'Key West,' and thus in 1860, the present head of navigation on the Missouri river was first reached by steamboat." The conditions under which steamboats operate on the Missouri river in the transportation of freight and passengers are so totally different from those on Eastern rivers that their design has to conform to the necessities of the case. The boats are of very light draught, and of great length and width in proportion to their depth. Their models vary widely from all the usual standard shapes, and are said to have been designed after the pattern of the mouth of the cat-fish. The engines are placed at the ex- treme after end of the hull, and are coupled at right angles to the shaft of the wheel, which is very much less in diameter than the wheels of a side- wheel boat, but extends nearly 'the whole width of the boat. The boilers are placed forward of the center. It is stated that a stern wheel boat will carry a load of 1,000 tons onjbut little more than half the depth of water required by a side wheelerjbr^the same load. Another important feature of the Missouri river boats is the spars used for lifting and dragging the boat over shoals and bars. In 1881, five lines of steamboats made their headquarters at Bismarck, Dakota, and twenty-one^boats plied between that town and points on the Missouri river, making, during the season of navigation, from one hundred and fifty, to one hundred and seventy-five trips. These boats carried into Montana 34,760,0(XTpounds of freight, valued at $5,214,000. The extensive railway construction"of the past few years throughout the Northwest, has had the effect of reducing the amount of river transportation; however, it is still quite heavy and boats ply regularly, during the season, between Sioux City and Bismarck, and Bismarck and the head of navigation. At present nine boats areln the trade'between Bismarck and Montana, and it is estimated that they will handle upward of 16,000,000 pounds of freight during the season of navigation. Navigation opens'about the 27th]of March and closes about the 10th of November. The Nationar.Governmenc annually expends large sums of money in improvements to the channel of the Missouri river, through the Territory. The Big Cheyenne, which drains the Black Hills region, contributes the largest volume of water to the Missouri river. The greater part of this stream lies within the boundaries of the Sioux Indian reservation, as also does that of the White, Bad, Moreau, and Grand rivers. The Cannon Ball river forms the northern boundary of this reservation. The Souris, or Mouse river is an erratic stream which, rising in the British Possessions, follows a southeasterly course to a point in Dakota sixty-five milessouth of the International boundary line, where it again RESOURCES OF DAKOTA. 75 turns northward and finally re-enters the Queen's Dominions. It flows for the most part, at a much lower level than that of the adjacent prairie, and its banks are covered with an abundant growth of timber. The Red River of the North forms the boundary line between Dakota and Minnesota from Lake Traverse to the Canada line. It is a deep, narrow and exceedingly crooked stream, traveling a devious course of some six hundred miles before finally emptying its waters into Lake Win- nepeg, Manitoba. The valley of the river is from sixty to eighty miles east and west by 300 miles north and south, every acre of which is the finest wheat land in the world. One hundred and eighty miles in length and forty miles in width of this valley, are situated in Dakota. The whea raised in the Red River valley is a grade unto itself, from the fact of its richness in albuminoids and its extreme dryness. It all grades No. 1, hard, and commands the highest market price. Steamers of two or three hundred tons burden (similar in construction to the Missouri river steamers, as described in the remarks on that stream), ply about eight months in the year as far up the river as Fargo, a distance of nearly 400 miles; and a part of the season, as high as Aber- crombie, fifty miles farther. Captain Alexander Griggs, at present the chairman of the Territorial board of railroad commissioners, built one of the first steamers on the river, — the "Selkirk," in 1871. From that date the number of boats in- creased rapidly, and in 1882, freight to the amount of 63,303,673 pounds was carried by water between Fargo and Pembina. The Government has annually appropriated a considerable sum for the improvement of naviga- tion on this river. During the summer months, millions of feet of pine logs are run down the Red River from the Red lake and Ottertail pineries in Minnesota, to the saw mills at Grand Forks. These mills manufactured 7,000,000 feet of lumber last season, and it is estimated that amount will be increased this year, to 20,000,000 feet, The James, or, as it is commonly known, the "Jim" river, which drains the country lying between the Red River and its tributaries of the north and the Sioux and Vermillion rivers of the south, on the east, and the Mis- souri river on the west, is not navigable. It has its source near Devils Lake in the northern portion of the Territory and flows in a southerly course to its junction with the Missouri in the vicinity of Yankton, on the extreme southern boundary of Dakota. The James, from source to mouth, has a length, counting its numerous bends and curves, of some five hundred miles, and is the longest stream wholly in Dakota, The valley of the James river is of great width and may be described as one vast prairie, bounded east and west by the horizon, and extending a distance north and south of nearly 400 miles. The fame of the fertility of its soil has had much to do with the rapid settlement of central Dakota, — by which is meant that portion of the Territory having the valley of the Mis- souri river for its western boundary, and bounded on the east by the val- leys of the Red and the Big Sioux. 76 RESOURCES OF DAKOTA. The valley of the James contains, not only the richest of farming land, thickly settled upon by well-to-do farmers, but along its course of many hundred miles, separated by easy distances, are located many of the most prosperous, enterprising and growing cities and villages of the Territory. The Big Sioux is an important stream, carrying a large volume of water, the drainage of innumerable lakes, ponds and marshes, situated around its head-waters in Kingsbury, Hamlin, Codington, Day and other counties. It flows in a southerly direction, forming the boundary line be- tween Lincoln and Union counties Dakota, and the state of Iowa, and empties into the Missouri at the extreme southeastern point of the Terri- tory. The Big Sioux river furnishes the best water power m the Terri- tory — equalled in all the Northwest only by the Falls of St. Anthony, on the Mississippi river at Minneapolis, Minnesota. At Sioux Falls, in Minne- haha county, the river falls through a series of cascades, a distance of ninety-one feet in running half a mile and supplies motive power for two large flouring mills, (one of which is seven stories high and occupies a ground floor space of 80x100 feet,) granite polishing works and other in- dustries. There is practically no limit to the power which can be sup- plied by the numerous falls of this stream, in the vicinity of Sioux Falls and Dell Rapids, when fully developed. The Vermillion river has its source in the northern part of Miner county and flows south, about midway between the James and Big Sioux rivers, through the counties of McCook, Turner and Clay and joins with the Missouri near the flourishing city of Vermillion. The waters of this stream pass through some of the best cultivated and oldest settled lands in the Territory. The Sheyenne is a stream of great length, having its source in Mc- Henry county, whence it flows in a southeasterly direction through the counties of Benson, Eddy, Nelson, Griggs, Barnes, Ransom ; thence running northeast through the counties of Richland and Cass, to its union with the Red. The region that is drained is more varied than that of the Red River valley, consisting of rolling prairies, diversified by ranges of low hills. The land is almost uniformally good; is easily tilled and highly productive. Many fine stock farms and ranches are situated along this stream. The Little Missouri river rises in Wyoming, northwest of the Black Hills, and flows in a northerly direction, through the western line of Da- kota's counties and empties into the Missouri, near the Ft. Buford Indian reservation. It is a considerable stream, and is noted for the extensive coal deposits along its shores and the fine grazing country through which it runs. Many thousand head of range cattle, fattened on the native grasses of the valley of the Little Missouri, are shipped annually to the Eastern markets. Innumerable streams of greater or less length flow into these large rivers, draining all sections of the vast Territory and furnishing, in their immediate vicinity, an ample supply of pure and sweet water for man and beast. RESOURCES OF DAKOTA. 77 WELLS. Where water is not to be had from a running stream, or from the num- erous hillside springs, abounding in many localities, it is generally very easily obtained by dug or driven wells. In most of the counties, a vein of excellent water is found, at a depth varying from a few feet to forty or more, by driving down an inch and a quarter gas pipe, to which is attached the usual style of driven well point and wire strainer. The operation is a simple one and inexpensive; a complete well of this sort costing from twenty-five to fifty dollars. In some localities the underground veins of water are at a greater depth from the surface and, in such case, it becomes necessary to dig wells, or bore one of the tubular pattern. The settler, in any part of Dakota, finds but little difficulty in obtaining a supply of good, pure water, either from some of the countless streams, lakes, swamps and ponds scattered throughout every county, or else by sinking a well of one of the patterns described. Many of the farms have wind-mills attached to the pumps and, by this means, supply a constant flow of fresh, cool water for both house and stable. Numerous artesian wells, from Yankton in the south, to Jamestown in the north, furnish every town of any importance, in the James River val- ley with a never-failing water-works system. In the counties bordering the Red River, artesian veins are found at a comparatively short dis- tance below the surface of the valley. The water is forced out, generally, with a pressure sufficient for fire protection and to carry it wherever de- sired. In response to inquiries sent out by this office, twenty-nine counties re- port artesian wells in successful operation — a sufficient warranty, one would imagine, for the expectation of obtaining this bountiful supply of water, together with power and fire protection — wherever, in Dakota, the proper effort is exerted. At the last session of the Territorial Legislature, (1887), a general law was enacted providing for the construction and maintenance of artesian wells in towns, townships, cities and counties, by the assessment of an equal tax upon the property owners and residents of the district or com- munity to be benefited — a provision which will undoubtedly lead to an extension of the advantages arising from artesian wells to a great many farming communities. A more detailed account of Dakota's artesian wells will be found on the succeeding pages of this publication. RESOURCES OF DAKOTA. AGRICULTURAL PRODUCTS.— WHEAT. Wheat is Dakota's principal agricultural product and will undoubtedly ever remain her chief staple, owing to the extremely favorable conditions which prevail within the Territory for raising the best quality of wheat at the lowest possible cost per bushel. The report of the Bureau of Chem- istry of the United States Department of Agriculture, 1884, contains the result of an analysis of 2,759 specimens of wheat, among which were in- cluded samples from every state of the Union, and many foreign coun- tries. The chemist, (page 70-79 of the report), says that the determination of the albuminoids, in connection with the size and condition of the wheat, settle, so far as a chemical and physical examination can succeed, the peculiarities and relative values of the samples submitted. The result of the analysis is to establish the fact by National investiga- tion that in the two most important desiderata, dryness and richness in albuminoids, Dakota wheat ranks the best of any grown on American soil, and probably averages the best of all the world. The following table is copied from the chemist's report: AVERAGE PERCENTAGE OP WATER AND ALBUMINOIDS IN THE COMPOSITION OF AMERICAN WHEAT. Locality. Water, per cent. DAKOTA 8.84 Pennsylvania 10.73 Maryland 10.52 Virginia 9.98 West Virginia 8.55 North Carolina 10.03 Georgia 10.00 Alabama ' 10.82 Ohio 10.68 Tennessee 10.24 Kentucky 10.83 Michigan 10.71 Missouri 9.80 Arkansas 9.56 Minnesota 9.96 Kansas 11.80 Texas 10.03 Colorado 9.73 Utah 9.17 New Mexico 9.30 California 10. 73 Oregon 9.74 Washington Territory 9.89 Highest Albumi- per cent. noids, Album'ds per cent. m anv specim'n. 14.95 18.03 11.44 15.58 11.65 14.53 12.10 14.00 10.94 11.03 10.43 12.43 11.78 14.00 11.29 13.65 12.83 16.10 12.50 16.63 13.15 14.53 11.67 15.23 11.56 14.00 12.95 13.19 17.15 11.15 12.25 13.14 15.23 12.73 15.94 10.15 10.50 10.50 11.73 10.94 12.78 8.60 9.47 8.23 8.75 RESOURCES OF DAKOTA. 79 The average percentage of albuminoids in the wheats of all the United States and British America is 12.15. In Dakota the average percentage is 14.95, leading every state and territory. The average percentage of dry- ness of the wheats of the United States and British America is 10.16. In this respect Dakota also leads every competitor with an average percent- age of only 8.84 of water in the composition of wheat grown on her soil. PAC-SIMILE OP FIRST PREMIUM AWARDED THE DAKOTA EXHIBIT For the best grade of hard wheat, World's Industrial Exposition, New Orleans, 1885. 80 RESOURCES OF DAKOTA. Commenting on the result of this investigation the chemist says: "as will be seen, the Dakota specimens are all extremely rich in al- buminoids; one containing as high as 18.03 per cent., which is the richest specimen ever analyzed in the United States." On page 111 of the report, the chemist has this to say of the result of an exhaustive analysis of samples of flours submitted from the various mill- ing centers of the country: "The Eastern flour is poorer in ni- trogen and gluten than any of the others. In fact, the flours follow closely the composition of the wheat which had been examined from the same parts of the country. Dakota makes a flour richer than any other, in gluten, in the same way that it produces a wheat of that description. The average of these ' Northwestern- spring wheat flours' is high, and in comparison with the rest of the country, they are the richest which have been analyzed. The hard wheats of the Northwest have furnished the country with a finer flour than it has before possessed, and in the baking experiments, the bread made from these flours excelled all others in quality." These experiments, carried on by authority of the National Govern- ment, establish two facts: First. That a bushel of Dakota wheat will make more bread than the same quantity of wheat raised in any other state or territory of the Union. Second. That the bread made from Dakota wheat flour contains more gluten and other of the materials which nourish and build up the human body, than bread made from any other brand. At the World's Exposition, New Orleans, 1884-5, Dakota was awarded first premium for wheat over competitors from all the famous wheat-grow- ing countries of the world. A fac- simile of the award is shown on the preceding page. Dakota's soil not only produces the finest wheat in the world, worth from five to ten cents more a bushel than the best grade of other markets, but it is raised at the lowest possible cost of production. From the Government census of 1880 we deduce the following figures: The average value of a farm in the state of New York, including land, fences and buildings, is $4,561 ; the average size of a farm in that state is 99 acres, making an average investment of $46 for every acre. In the state of Ohio the average value of farm property is $44 per acre. In Da- kota the farmer has an average investment in his farm property of only $5.90 per acre and he raises a finer grade of wheat than does the Eastern farmer, with ten times the amount invested and with a corresponding in- creased annual outlay for taxes and interest on the investment. A prominent citizen of the Territory — one who has heavy interests in the lands of both Dakota and the state of New York, is authority for the following comparison : "A farm situated in western New York, and containing say 160 acres of land, will pay a tax of from $75 to $100 per annum, while a fairly well im- proved farm in Dakota, of the same acreage will be taxed but from $25 to RESOURCES OF DAKOTA. 81 $40; here, in the item of taxes alone is a margin of saving to the Western farmer of about $50 per year. A mortgaged farm of say about 160 acres in western New York usually carries a mortgaged debt of not less than $5,000; the interest upon this debt at the rate of 5 per cent., (the lowest rate made in that section,) is $250 per year. Now, on the other hand, the average mortgage upon a fairly improved farm of 160 acres situated in Da- kota, is not more than $800, and, at the highest rate of interest now ex- acted in this Territory upon real estate mortgage security, namely 10 per cent., the interest upon a Dakota mortgage would be $80 per annum. Thus we see that in the matter of interest there is a difference in the favor of the Dakota farmer of $210 per year, which added to the $50 saved in the way of taxes, makes a net yearly saving to the Dakota farmer of $260, not by any means an insignificant amount at this period of meager margin of profit in general farming operations throughout all sections of this country." The East can never compete with Dakota in the cheapness of the pro- duction of a bushel of wheat, no more than can she raise wheat of an equal quality. The following estimates of the actual cost of raising a bushel of wheat in Dakota, during a season of average conditions of favorableness, will be of interest to the intending settler: Mr. Henry Sleight, a reliable farmer of Stutsman county, says: " In May and June, 1881, I broke 113 acres, with 12-inch walking plows, about three inches deep and back-set in July and August, about an inch deeper than the breaking. Last spring, as soon as the frost was out of the ground suf- ficiently, I went over it once with a disc harrow and seeded it with Scotch Fife wheat, one and a half bushels to the acre, using force-feed broadcast seeders, following with common harrows twice over. The seeding was completed about the middle of April. The wheat came up quickly and evenly and gave promise of an extraordinary crop until the July drouth, which checked it in heading and materially reduced the yield. Harvest- ing was done about the middle of August, and threshing from the shock in September. The crop on the 113 acres was 3,912 bushels, over 34J bushels per acre. "The cost of producing the crop, as given below, is the actual expense for labor — $25 per month wages and 50 cents a day board for men, and 16f cents a day for feed for each horse. In threshing, five additional men were employed at $2 per day, which is also included in the cost of threshing. SUMMARY. Seed wheat, 169J bushels, at 75 cents $ 127 13 Pulverizing with disc harrow, man and 3 horses, 5£ days 10 84 Seeding, man and two horses, 9h days ....... 17 00 Dragging, man and two horses, 11 days 21 67 Harvesting, two men and three horses, nine days 29 25 Binding twine 41 00 Threshing and putting in granary 152 50 Stubble plowing 85 88 Total $ 485 27 82 RESOURCES OF DAKOTA. " By proportioning the taxes assessed last June,[the interest on the cost of the farm, stock, machinery and other equipments, and on the expense of operating the farm, for the current year at 6 per cent., the wear and tear of stock, machinery, etc., together with the expense of keeping the stock during the winter, the cost of production will be increased about $345— making a total of $830.27. "That the statement may be better understood, I will add that the farm contains 800 acres; about 700 acres under cultivation, 80 acres of fine hay meadow and 20 acres taken up by highways. The cost of the land, build- ings and breaking was about $20,000, and of the stock, machinery, imple- ments, etc., about $6,500. As the land was all comparatively free from noxious plants, no summer fallowing was done this year on the farm, and the teams were engaged nearly two months — from the last of May until the latter part of July — in breaking and fallow-plowing for others." The cost of raising a bushel of wheat in this instance, after adding to the farm expenses an allowance for taxes, interest, wear and tear of ma- chinery, etc., was but 21|- cents. Had it not been for the July weather, Mr. S. is certain his yield would have been 40 bushels per acre instead of 34J, which would have materially reduced the cost per bushel of produc- tion. The following shows the actual result of the cultivation of 155 acres in 1885 — an unfavorable year: Plowing 155 acres, fall of 1884 ..$ 194 00 Seed 119 25 Interest on above, 10 months at 10 per cent 25 85 Seeding 155 acres 155 00 Rolling 30 00 Interest on above, 4 months 6 08 Harvesting and shocking 232 50 Threshing and delivering at elevator, 11 cents per bushel 357 50 Tax on land 25 00 Interest on money invested in land 130 00 Total cost $1,275 18 The yield was 21 bushels to the acre, a- total of 3,255 bushels. The cost of raising wheat as per above statement was about 36 cents per bushel. W. W. Warren, Esq., general manager of the Grandin Brothers' farm, at Mayville, Traill county, says that the cost of raising a bushel of wheat on that farm, including interest on capital, wear on machinery, Wages, in- cidentals, etc., is a little less than 24 cents per bushel. Hon. Lauren Dunlap, late Commissioner of Immigration for Dakota, prepared the following table on the cost of wheat production in the Terri- tory, as showing the average expense to the ordinary farmer, based upon actual results within the knowledge of this office: RESOUKCES OF DAKOTA. 83 COST OF PRODUCTION PER ACRE. Plowing $1 00 Seeding, 1£ bushels at 80 cents 1 20 Cultivation and sowing 50 Harvesting and stacking 1 25 Threshing and marketing 2 00 Total ." $5 95 EXAMPLE. Plowing 160 acres, at $1 $ 160 00 Seed for same, 240 bushels, at80 cents 192 00 Cultivating and sowing, at 50 cents per acre 80 00 Harvesting and stacking, at $1.25 per acre 200 00 Threshing and marketing, 3,200 bushels at 10 cents 320 00 Interest on capital invested, $2,000 at 10 per cent 200 00 Total $1,152 00 Cost of production per acre, counting a yield of 20 bushels $ 7 20 Cost of production per bushel 36 The highest estimated cost of the production of a bushel of wheat in any one of the statements quoted — 36 cents — is lower than the estimated cost of production in the great wheat growing country of India, and is at least 50 per cent, below the average cost of production throughout the United States. An official document estimates the cost of growing wheat on manured and irrigated land in India, at a little under a shilling per bushel, or in- clusive of rent, Is. 6d., or 36J cents. This includes seed and threshing. The statistician of the Department of Agriculture — Hon. J. R. Dodge — says: "While India is the principal competitor of the United States in the world's markets, her importance as a competitor is greatly overrated. The occurrence of a 'famine year' would reduce to zero her exports. So fixed are the industrial usages of the people that great enlargement of the wheat area is next to an impossibility ; there has been no material increase as a result of the exportation of the surplus of the last ten years. The ex- tension of railroad mileage has facilitated the shipping of the surplus of good years which would otherwise have been pitted to eke out subsist- ence in famine years. It might not be fair to say that these shipments have produced no effect; if any, it has been very small. The exports of ten years include nearly the sum of India's record of exportation, and would scarcely equal the crop of an average year. A 10 per cent, surplus that cannot be depended on in a crop half as large as ours, cannot take the place of our surplus, which is more than half as large as the India crop." 84 RESOURCES OF DAKOTA. He is also authority for the statement that while the cost of production under favorable circumstances, and in the best localities of India, may be 35 to 40 cents per bushel, wheat can rarely be brought to the"principal markets and sold for less than 60 cents. Consul-general Mattson, at Calcutta, says that the native of India can afford to sell his wheat at the nearest market place, if within a day's jour- ney of his home, for 50 to 60 cents per bushel ; but when it does not bring that price, or very near it, he either consumes his small supply, or stores it in a hole under the ground until a more favorable time shall come. English wheat-growers claim that it costs about $40 an acre to grow wheat in England, and that they must get from 40 to 45 shillings a quarter, or from $1.09 to §1.36 a bushel for their grain to make the growing of it profitable. Dakota has the soil, the climate and every advantage in her favor as a competitor for supplying England, the great wheat market of the world, with bread, and whenever our intelligent, thinking farmers grasp the sit- uation and till their lands as do the farmers of Europe, or even the farm- ers of the older settled areas of our own country, we shall at once attain, and forever maintain the prestige of wheat producers of the globe. If the Dakota farmer can afford to raise wheat under the general hap- hazard style of farming, which brings him only a third of the yield the land ought to and would produce with skillful management; with a reck- less investment in farm machinery and an utter disregard of caring for it after it has been purchased, as has characterized his operations in the past; and with no thought of husbanding his crops for a favorable market but, acting in concert with all his neighbors he throws the entire season's yield, as soon as threshed, on the hands of the grain specula- tor, which, as a matter of course, affects the markets disastrously — and still compete with the pauper-labor of India and the careful, painstaking farmer of Europe, what wealth and prosperity is in store for this same farmer when he shall, by means of scientific agriculture, double the yields of his fields; when he shall act judiciously in creating indebtedness and sensibly in housing his machinery ; when he shall provide a storage- house for his grain, and compel the grain buyer to seek him nstead of put- ting himself entirely within the power of the elevators as now, and, last of all, when he shall diversify his crop and combine stock-raising, dairy- ing, and the other valuable adjuncts of farming with his yearly wheat ventures! The yield of wheat in England is from twenty-six to twenty-eight bush- els per acre ; in France twenty-four, — about twice as much as the yield in the United States. And why? The answer is obvious — this high yield i& the sole result of science, and thrift, applied to farming operations. The natural fertility of the soil does not necessarily control the yield of a coun- try. No where on the globe, is there a wheat growing soil to compete with that of the Red River valley — and yet the poor, worn out lands of some of RESOURCES OF DAKOTA. 85 the Eastern states are caused, through skilled effort, to bring forth heav- ier crops than this favored spot. The farmers of New England cultivate a soil of sand and gravel, but by constant tillage and the use of fertilizers, this same land has averaged for the past five years a yield of 30.8 bushels of corn to the acre, while the rich loam of the Missouri valley — where nature has furnished every aid to increase the farmer's wealth, — returned but 29.8 bushels. It costs the Dakota farmer quite as much for seed, labor, taxes, living,, etc, to raise twelve bushels of wheat to the acre as if he had raised double the amount. An increase of a single bushel in the average yield of wheat means over 12,000,000 to be distributed among the farmers of Dakota — every cent of which, outside of the cost of threshing and marketing, is clear gain. ^Statistical research shows that a crude agriculture is not abundant in product, and that it is compelled to pay high interest on borrowed money. A low grade of farming is cursed with mortgages and mildews, with in- sects and ignorance. Uncertainty broods over its harvests, and famine decimates its people. Famine is unknown in a country of advanced agri- culture, though a fourth of its people only may be engaged in rural pro- duction. On the contrary, millions famish in India, while most of its peo- ple are in agriculture. * * * * * * * In seasons unfavorable to production, the money value of skill and science in agriculture is immensely enhanced. It is often remarked that farmers receive as much for a very small crop as for a very large one. In 1881, 1,195,000,000 bushels of corn were worth $760,000,000; in 1884, 1,795,- 000,000 bushels were valued at $641,000,000; a small crop was worth 63.6 cents per bushel, a larger one 35.7 cents. A crop of cotton once sold for $40,000,000 less than the previous one, which was more than 1,000,000 bales larger. Nevertheless there is disaster in a small crop. The failure is un- equally distributed. The few advanced farmers grow nearly full crops, and receive larger revenues than usual; the many unskilled and careless suf- fer disastrous reduction of yield and quality, and fail to make return for seed and labor. Given unscientific agriculture, with an inauspicious sea- son, and the poor may grow poorer, while the scientific farmer, in the same year, may grow richer. * * ■ * # * -* Among the results due to applied science in the work of agriculture, the following are prominent: First. Fertility is increased; the rate of yield is greatly enlarged; labor is lightened; the laborer is less a 'beast of burden, ' and more a master of machinery. Second. The margin of profit is increased, or rather, one appears where none before existed. Third. Production is equalized — there are fewer gluts of certain pro- ducts, and greater variety in production. *Hon. J. R. Dodge, Statistician, Department Agriculture, Washington, annual re- port, 1885. 86 RESOURCES OF DAKOTA. Fourth. Disasters of primitive agriculture are partially averted — drought by deep and thorough culture, excessive rainfall, by drainage; in- sects are less numerous with rotation, and their injuries are outgrown by vigor of vitality and strength of growth; blights and other maladies of veg- etable physiology are avoided by amelioration of the soil and cultivation in harmony with the conditions of healthful growth. Finally, by application of the discoveries of science, the farmer unites brain with brawn in rural production, labor loses its drudgery and ac- quires effectiveness, the profit and pleasure of agriculture are advanced, the public wealth and welfare are promoted, and a country life, whatever its previous charms, is far better worth the living. The wheat crop of Dakota in 1880, as recorded in the annual report of the Department of Agriculture, was 80,704,000 bushels, the product of 2,675,350 acres, or an average yield of 11.5 bushels to the acre. But this statement is almost as inaccurate and misleading as others referring to Da- kota, on page GO of the same official work, wherein it is said that "the varieties of spring wheat grown in southwestern (?) Dakota have a world- wide reputation for producing the best quality of flour!" that "our princi- pal market crop is flax!" and that " tomatoes and melons rarely mature on account of frost! ' " The truth of the matter is the Territory has never re- ceived proper credit for the crops she has raised — through the fault, chiefly, of her own weak and inoperative statistical law. As this law now stands, but a small proportion of the assessors of the Territory comply with its terms, and the Commissioner of Immigration is dependent almost solely on the kind co-operation of county auditors and clerks, city officials and voluntary reporters selected from among the farmers, for statistical information regarding the season's crops. Careful computations, verified in every instance by a number of reliable and competent citizens of each county, make the average sown to wheat in 1886 exceed the amount credited to Dakota in the report of the Com- missioner of Agriculture by 574,141 acres, or a total of 3,249,491. This would have given us, even at the average yield computed in his report, a crop of 37,369,146 bushels, or an excess of nearly 7,000,000 as compared with the estimates of the Department of Agriculture. Dakota was given the sixth place in the rank of wheat producing states and territories last year, whereas she was really entitled to the fourth — her yield of this cereal having been exceeded in quantity by the three states only of Ohio, Indiana and Minnesota — a splendid showing when we consider the fact that the season throughout the Northwest was one of the most unfavorable ever recorded. But it is the wheat crop of this year, (1887), which establishes Dakota in the lead, beyond all fear of # competition, as the greatest wheat producing country of the Union. Nearly two months' labor of this office have been spent in the collecting and compiling of several hundred reports and estimates of the season's crop area and yield per acre, received from leading farmers and reliable RESOURCES OF DAKOTA. 87 TABLE SHOWING THE WHEAT CROr OF DAKOTA In comparison with each state and territory in the in 1886, Union. Rank. States Bus/iets. 43 MASSACHUSETTS, 1 17,000 42 CONNECTICUT, I 36,000 41 WYOMING, s 63,000 40 NEVADA. ■ 72,000 39 NEW HAMPSHIRE, 38 MISSISSIPPI, 169,000 173,000 37 ARIZONA, 36 VERMONT, 297,000 35 MAINE, 34 NEW MEXICO. 410,000 600.000 921.000 33 SOUTH CAROLINA. 936,000 32 IDAHO, 31 DELAWARE, 30 MONTANA, 1,039,000 1,177,000 1,509,000 29 ALABAMA, 28 UTAH, 27 GEORGIA, 26 ARKANSAS, 25 NEW JERSEY, 24 COLORADO, 23 WEST VIRGINIA, 22 NORTH CAROLINA, 21 TEXAS, 20 VIRGINIA, 19 MARYLAND, 18 WASHINGTON TER.. 17 TENNESSEE, 16 NEW YORK, 15 OREGON, 14 KENTUCKY 13 KANSAS. 12 WISCONSIN. 11 NEBRASKA, 10 PENNSYLVANIA 9 MISSOURI, 8 MICHIGAN, 7 ILLINOIS, 6 DAKOTA, 5 IOWA.' 4 CALIFORNIA 3 INDIANA 2 oino 1,529,000 T,541,000 1,690,000 1,815.000 2.260,000 2,419,000 3,061,000 8.209.000 5.8*3.000 5,581,000 7,194.000 7,560,000 8.024.000 11,093,000 11.133,000 12.405.000 14.556.000 14,725,000 ! MINNESOTA 27,562.000 30,704,000 32.455. ( 00 "" 36, 165. 009 40,255.000 ~ 40.302. 060 42,856,000 88 RESOURCES OF DAKOTA. citizens, representing every county of the Territory. The acreage and yield for each county was obtained by taking the average of a number of estimates from different sources of the same locality, and, wherever pos- sible, this result was again verified by the assessors' annual return of sta- tistics. The totals, therefore, as herewith published are believed to be as nearly accurate and reliable as it is possible to make them. The showing is simply astounding, and almost beyond comprehension, viz.: a yield in 1887 of 62,553,499 bushels of wheat, from an acreage of 3,818,754, or an average of 16£ bushels to the acre. Dakota, in 1887, raises more wheat than was ever credited to any one state of the Union for a season's yield, or about one-seventh of the entire wheat crop of the United States in 1886 — or almost one-thirtieth of the wheat crop of the world. Is further argument necessary to convince the public of the certainty of Dakota's future and of the permanence of her growth and development? The yield of wheat in 1887 is an increase of about 100 per cent, over the crop of 1886, as computed by the Department of Agriculture, and a gain of about 70 per cent, over the estimates for the preceding year, of this office. The acreage sown in 1887 is an increase of about one-fourth, as com- pared with the published report of the Commissioner of Agriculture in 1886, or about one-fifth more than the estimated acreage for that year as made by this office. The average yield per acre in 1886 was 11.5 bushels; this season it is 16£, or a gain in the yield of over 40 per cent. Dakota, still a territory, with her resources but partially developed, with but one-thirtieth of her area sown to grain, has even now taken rank far ahead of the famous wheat-growing states of the Union, and leads all competitors in the quality of the grain produced and the cost of produc- tion. The eventualities of the near future, when the millions of acres of vacant land are peopled, and add their product to augment the Territory's grand total; when farmers apply lessons of science and economy to the operations of agriculture, and when the completion of the net-work of railroads now projected give the product of the most distant farm an out- let through the lakes to the sea-board at one-fourth the present cost of transportation, cannot fill the mind with a single hope of wealth, grand- eur and prosperity for Dakota which will not be realized. Dakota's prairies will furnish the bread supply of the Nation; the best article at the lowest price. The soil Of Dakota requires no fertilizer — her climate obviates any need of irrigation ; there are no stones or trees to be cleared from the farm and the smooth, level prairie permit of the use of many labor-saving farm tools, which the rough land and the small area of Eastern farms pre- clude. Furrows are run for miles without a turn, and it is a day's journey with a self-binder to cut the opening swath around one of Dakota's bo- nanza farms. RESOURCES OF DAKOTA. 89 Dakota's wheat is all of the spring variety, and therefore the farmer is not subjected to the dangers of losing his crop by winter-killing, as hap- pens frequently to the winter wheat area. Damage to the crop by rust. Hessian fly, or chinch-bug has never occurred in the history of the Terri- tory. The entire wheat crop of the United States could be grown on Dakota's wheat land, antl even then there would remain a vacant area larger than the combined surface of the states of New York, Maryland, Vermont, New Hampshire, New Jersey, Massachusetts, Connecticut, Delaware and Rhode Island. The following table shows the amount of wheat inspected at the princi- pal grain depots of the United States during the year ending December, 1886: Locality. Minneapolis. Detroit Chicago Kansas City. Milwaukee... New York... No. of cars. 59,322 17,547 34,160 4,741 14,472 18,110 The advantage and saving of water transportation, as compared with a long land haul in the movement of grain toward the great markets of the world, is too well known to need additional argument. Wheat was car- ried from Chicago to New York, by lake and canal, during the season of 1886, for an average price of nine cents per bushel, and to Liverpool from New York, by ocean steamers, for an average tariff during the year of 7 J cents. The rate on grain by rail betw r een Chicago and New York, during the same period, was at no time less than 25 cents per bushel, and aver- aged for the year about 26 cents — nearly three times heavier than the lake and canal rate. During the year ending July 31, 1887, 38,500 car loads of wheat were re- ceived at Duluth, being considerably more than was handled at either Chicago, Detroit, Milwaukee, New York or Kansas City, and exceeded only by Minneapolis, for the year 1886. Since the opening of navigation, (1887), in less than fifty days, there had been shipped from Duluth 7,000,000 bushels of wheat — a wonderful increase over the shipments for the same length of time of any previous year. These facts are presented as a proof of the rapid strides taken by this new competitor in the direction of the leading wheat-shipping point of America, and as emphasizing the great advantage to the farmers of Da- kota of the many railway lines, already completed and under construc- tion, connecting the Territorial cities with Duluth, shortening, by more than one-half, the land haul from the wheat fields to the lakes. The time is rapidly approaching when the entire surplus wheat crop of 90 RESOURCES OF DAKOTA. the Northwest will find its way to the elevators of a city destined to be- come the greatest grain mart of the world, distant but 200 to 350 miles from the wheat fields of Dakota, and when our surplus grain will be shipped to the seaboard at less than the present cost of transportation to Chicago. The president of one of the leading railway corporations of the United States, recently uttered the following prediction: "It wftl not be long until points in Dakota, within 500 miles of Duluth, will be sending wheat from their stations to Buffalo for 15 cents per bushel." This means that wheat raised on Dakota soil at a cost of from 23 to 36 cents per bushel, with an investment of $5.90 per acre, will bring in the local market, (when freights to the seaboard are lowered to this extent) , almost the same price that the Eastern farmer receives for his, raised at double the cost of production and on land representing ten times the capi- tal invested. The following table shows the wheat crop of the world in 1880: Countries Bushels. America: United States 457,218,000 Canada | 37,219,234 Argentine Republic and Chili 28,800,625 Europe: Austria-Hungary \ 143,001,488 Belgium 1 18,514,688 Denmark 4,731,531 France I 299,107,620 Germany j 82,000,000 Great Britain and Ireland' I 65,285,353 Greece 4,937,250 Italy I 129,412,133 Netherlands ! 4,937,250 Portugal 8,228,750 Roumania ! 22,629,063 Russia ! 213,907,084 Servia j 4,525,813 Spain 131,660,000 Sweden and Norway ! 2,468,625 Switzerland ...i 1,645,750 Turkey ,.. 41,143,750 Australasia j 22,258,146 India ■. I 258,317,632 Egypt | 16,457,500 Algeria ; ! 32,915,000 Total 12,031,322,285 Dakota's wheat crop, just harvested, is greater than the whole yield in 1886, of Turkey in Europe ; nearly double the product in 1886 of either Canada or Algeria; more than twice the total annual yield of the Argen- tine Republic and Chili combined, or of either Roumania or Australasia, and three times the amount raised last year in either Belgium or Egypt. The entire 1886 wheat crop of the following countries, viz.: Denmark, ♦RESOURCES OF DAKOTA. 91 Greece, The Netherlands, Portugal, Servia, Switzerland, and Sweden and Norway, when added together, makes but one-half the yield of Dakota in 1887. Indeed, the statements received by this office — and they are vouched for as being trustworthy and reliable- — prove that our wheat crop this season is less than 3,000,000 bushels below the whole product of Great Britain and Ireland, as last recorded. The official record of imports of wheat into the United Kingdom for the first half of the present year, (1887) , shows a large increase in the pro- portion furnished by the United States, 68 per cent, against 54 per cent. in the first six months of 1886 and 1885. Counting flour as wheat, the pro- portion is 73.5 per cent, against 60.8 in a similar period of 1886, and 60.6 in 1885. Analyzing the table, there is found a great reduction in receipts from Russia, a decrease from India of 20 per cent, as compared with the first half of last year, and a decrease from Australia. The quantities of wheat imported from January to June, inclusive, with value and average price, expressed in the measures of this country, are as follows: Countries. Bushels. Dollars. Russia 2,782,608 1,113,629 32,718,276 1,063,011 6,725,790 3,650,170 2,847,311 1,226,154 34,870,614 1,101,367 6,670,429 3,726,848 Germany United Statas Chili India Other countries Total 48,053,484 50,442,723 Value per bushel. $ 1 02 1 10 1 07 1 04 99 1 02 1 05 The value of wheat from this country is eight cents per bushel more than that from India, and five cents more than Russian wheat. It is higher than that of any non-European country, and yet the quantity fur- nished is twice as much as that supplied by all other countries. Of the imports of flour as wheat Austria furnishes a small quantity, and Germany still less, while the receipts from the United States constitute 86 per cent, of the importation. ***'■-*.'***'* The present indications point to a more than average European crop. It was late nearly everywhere, perhaps two weeks on an average at the be- ginning of June, but in growing condition, and its advancement since has been rapid. The Russian and Austrian crops especially are of fine promise. That of Spain is mediocre. In Germany, France, and England, reports are generally favorable. The India crop, harvested a few months ago, will be 20,000,000 bushels less than the preceding, say 238,000,000 bushels. Australasia will probably produce 15,000,000 bushels more than in 1885-'86, or 37,000,000 bushels. The product of the world promises to be quite as much as for each of the two preceding harvests. A close calculation cannot be made while so 92 RESOURCES OF DAKOTA. much uncertainty exists as to the harvest test of present prospects in cer- tain countries. Present indications do not promise material increase in prices; they certainly do not demand lower prices. The demand from Europe should be less than usual, if crops of Western Europe are as good as reported, though stocks are low; but if prices con- tinue low as at present, their replenishment must increase the sum of purchases. It appears that America is still in advance in the competition, furnishing bread to the world at lowest rates with ease and cheerfulness, and probably will have wheat to sell should prices run materially lower. It would be better, however, to sell less wheat abroad, and supply the de- ficiency in barley now obtained by importation, or produce other crops for home consumption at better profits. * The rapid development of the agricultural and other resources of Dakota in so short a period is fairly represented by the following comparative table showing (from official sources,) the wheat crop of the Territory in 1860, 1870, 1880, 1885 and 1887. WHEAT CROP. Bushels. 1860 1 945 1870 ■Hi 170.662 1880 | 2,830,289 1885 B£S 38,166,413 1887 ||§ £H^2,553,499 * Report of the Statistician, Department of Agriculture, Washington, August, 1887. RESOURCES OF DAKOTA. 93 CORN. Dakota's leading interest must always be that of the farmer's. The great extent of magnificent soil, of cheap lands easily tilled, and yielding a bountiful return for the husbandman's efforts, is rapidly crowd- ing the Territory toward her eventual position as the garden spot of the Nation; the depot for the food supplies of the Union. But in this agri- cultural country, to bring about the full measure of success, there must be an encouragement of the farmers to diverstfy their productions. "Man cannot live on bread alone," — neither will the farmer be the most success- ful who confines his operations in the one direction of raising wheat. The experiment was tried in the settlement of Illinois, of Wisconsin, of Minnesota, of Kansas, and Nebraska, and the failures marking the at- tempts to grow wheat exclusively there was a lesson the Dakotaian has wisely heeded. The homesteader or preemptor, as a general rule, begins operations on his new home with a very limited capital: — the cost of breaking the land, of erecting buildings, and the purchase of farm implements must be met by the immediate sale of his yearly productions, and no crop is so readily changed into cash as wheat. As a result the new comers to Dakota were, perforce, wheat-growers. But now that the farm has been developed, and the heavy expenditures of the first years are lessened' — he is investing every dollar of his surplus earnings in cattle, horses, sheep and hogs, and in dairying and cheese making. The corn market is seldom or never overstocked. In the cultivation of this farm product there is little or no competition of other countries, and if the price is unsatisfactory the former is never at a loss to find profitable and varied uses for his surplus at home. Of corn and other feed for farm animals only a small portion of the crop comes within reach of the speculator, whereas, with wheat, nearly every bushel is 'shipped from the farm, and, as an official of the Government says, "is a prey to speculation every step of the way from the first coun- try market to the consumer's larder 1,000 to 5,000 miles distant, running a long gauntlet of forwarders, carriers, commission and elevator men, and buyers on speculation, whose charges all come out of the price fixed by the world's competition, leaving to the grower whatever remainder the rapacity of this army of distribution may have been unable to confiscate." 04 RESOUKCES OF DAKOTA. TABLE SHOWING THE CORN CROP OF DAKOTA IN 1886 In comparison with each state and territory of the Union. Rank, States. Bushels. 45 NEVADA, 1 92,000 44 MONTANA, 1 22,000 43 IDAHO, 1 42,000 42 ARIZONA, I 67,000 41 WASHINGTON TER., ■ 88,000 40 OREGON, EH 178,000 39 UTAH, ■ 2J7.000 RHODE ISLAND, COLORADO, NEW MEXICO, MAINE, NEW HAMPSHIRE. MASSACHUSETTS, CONNECTICUT, VERMONT, NORTH CAROLINA, MICHIGAN, WISCONSIN. ALABAMA, GEORGIA. IOWA, 438,000 938,000 973,000 989,000 1,364,000 1.922,000 1,992.000 2.058.000 30 DELAWARE, WB^Sl BB 3,590,000 29 CALIFORNIA, Ifflfffilllfffl MB 4,262,000 28 FLORIDA, BSjgSIl B 4,597,000 27 NEW JERSEY, KBWWWWWWfl IB 9,418,000 26 SOUTH CAROLINA. IS 13,318,000 25 LOUISIANA, SB 14.010.000 24 MARYLAND, ffi^PI^P^ Hill 15.039.000 23 WEST VIRGINIA. g|BH 15.194.000 22 DAKOTA, m&AM&mt BB 15,305,000 21 MINNESOTA. EffgjflMTjffHi mSi 19.905.000 20 NEW YORK. BHBSH BB 22.426,000 19 MISSISSIPPI. gBI 25.507.000 27,215,000 27,635,000 28,493,000 28,893,000 31,197,000 13 VIRGINIA, IWirn 32,793,000 12 PENNSYLVANIA, — 40,545,000 11 ARKANSAS. B 42,140,000 10 TEXAS, HM— WBBH HB 69,213,000 9 TENNESSEE, B 73,314,000 S KENTUCKY jjB SS^BB B 88,758,000 7 OHIO, B 96,204,000 106,129,000 1 ILLINOIS, 198,847,000 209,818,000 RESOURCES OF DAKOTA. 95 The rich and distinctive soil of the Red River valley, especially en- dowed by nature for the production of wheat, the equal of which is not grown elsewhere in the world ; with never a disastrous failure marking its history of phenomenal yields; with its special farm tools, large areas, and systematic culture, whereby the cost of production is lowered beyond fear of competition, — must and will continue in the future, as in the past, to grow a third of the entire wheat crop of the Territory. Farmers there have grown rich by confining their operations solely to the growing of wheat, and the advantages of its particular soil are such that the Red River valley must always maintain its present prestige of raising the best and cheapest wheat known to the markets of the world. But the farmers elsewhere in Dakota have learned that there is not the profit in growing wheat exclusively — even though the yield should be ever so heavy, and the quality unexcelled, — as accrues from a diversity of products, the rais- ing of corn, oats and grass, — crops which can be marketed at home, in the way of meat, butter, cheese, etc. Wheat will always be a part of the farmer's crop in every section of the Territory, and an extremely profitable one, too, when by a rotation of uses the soil is made to yield him a better, surer and larger return than even now, and when his live stock interests shall relieve him from the necessity of crowding his wheat crop on the low markets of the early fall. There can be no more certain and positive indication of the success and wealth in store for the farmers of Dakota, than is displayed by the pro- gress of the past three years toward a diversity of crops. It is with a marked degree of satisfaction those, who are interested in Dakota's welfare, observe the increased area sown from year to year in corn, oats, barley, and the tame grasses. It means that the Dakota farmer has profited by the failures recorded in the early history of all the West- ern states, and is too wise and intelligent to place his dependence on the yield of a single cereal. It means that he has become a stock-raiser as well as a tiller of the soil. A studv of the tables in another part of this publication, exhibiting the rapid increase each year of the numbers and value of the farm animals in the Territory, in connection with the enlargement of the area planted to corn and other stock supplies, is a convincing proof that the tillers of the soil in Dakota are following in the footsteps of the successful farmer of Iowa and Illinois, and have adopted the plan of mixed farming and of diversifying farm products. The encouragement and growth in the future of an investment in hogs, cows, sheep and horses, that must follow as a natural result of the ven- tures of those who have already demonstrated its value, have made doubly certain the success which will always attend the efforts of the farmer in Dakota. The time is remembered when Dakota was considered as lying outside of the corn belt, and the same was thought to be true as regards the adaptability of the soil and climate for the raising of wheat; but, as the supposition that wheat could not be grown on Dakota soil has been 96 RESOURCES OF DAKOTA. demonstrated to be without foundation, just so is experience teaching the world that the corn area of the Northwest extends far beyond the bound- ary, to which it w T as confined a few years ago. With a soil beyond comparison and a climate akin to that of the great corn growing states of the West, the wonder is that the question of rais- ing corn in Dakota should ever have been clouded with a doubt. Fortunately many of the thrifty and enterprising farmers, who have made new homes in Dakota, were stock-raisers in the states from which they came, and had learned the value, to the farmer, of connecting stock interests with a diversity of crops. They soon demonstrated that Dakota's soil and climate would not only raise the finest wheat in the world, but was also equally as well adapted for the cultivation of corn. We have seen the corn area extended from the few counties in the ex- treme southeast, until to-day, the acreage planted in Dakota will almost equal that planted to corn in one-half the states of the Union. Corn is now a leading crop with the farmers of every county in the southern and central portion of the Territory, of the Black Hills, and is raised in con- siderable quantities even in the counties of the north, especially in the counties bordering on the Missouri river. Each year witnesses the widening of the corn belt in Dakota, and the gradual conversion of the farmers of the most northerly localities to the belief, because of actual results, that corn can be grown anywhere in the Territory. The extraordinarv increase of the corn acreage and product will be bet- ter understood by a study of the following exhibit: CORN CROP. Bushels. 1860 1 20,269 1870 SB 133,140 1880 Hmm 2,000,864 188.1 ■ 7,800,593 18=7 ■ ■■24,511,726 The yield of corn for 1887, as stated above, is the report of several hun- dred correspondents, including farmers, merchants, and other leading citizens, representing every county of the Territory. The acreage and yield was obtained by counties, and for^each an aver- age was taken of several different estimates covering the same locality. Whenever it could be done the crop statistics were compared with the assessors' returns for the year. The result of these compilations shows an area planted in corn, in 18S7, of 608,807 acres, yielding a crop of 24,511,726 bushels, or an average yield for the Territory of forty bushels to the acre. The estimates in the past of the Department of Agriculture regarding the crops of the Territory cannot be relied upon for accuracy. We have shown that the Commissioner, in his report for 1886, gave the area sown to wheat in Dakota below what it actually was; but with corn, his figures, are altogether too high. RESOURCES OF DAKOTA. 97 From careful estimates, verified in every instance by reliable and intel- ligent citizens of each county it is learned that the area in corn in Dakota in 1886 was 400,640 acres, or, about 262,000 acres less than was published by the Commissioner of Agriculture. In the three years from 1884, the corn crop of Dakota has more than trebled in quantity, with the certainty of constantly increasing, in the future, this established ratio of progress. Dakota in 1887 raised more corn than the entire product in 1886 of either the state of New York, Minnesota, Maryland, South Carolina, New Jersey, Louisiana, West Virginia, California, or seventeen other of the states and territories. The crop was planted in good season under extremely favorable cir- cumstances and had the advantage throughout the growing months, of weather especially suited for the growing of maize. The ears are un- usually large, filled out to the very tips and, as regards quality, cannot be excelled by the corn growing in any state in the Union. The entire crop has matured without the slightest damage from frost or the ravages of insects and is declared by the farmers everywhere, — of the Black Hills, of the south and central sections of the Territory and of coun- ties in the very north to have furnished a better general average of con- dition, of yield and of profit, than was ever before realized from any farm product, of an equal investment. Of the quality of the corn raised in Dakota, the same is true as has been said of the quality of our wheat. It is extremely rich in albuminoids and nitrogen (the nourishing properties) and in this respect is above the average of corn grown in the states, and the general average of the com- position of American corn. The following table is copied from page 87, report of U. S. Department of Agriculture, 1884, and is the result of an analysis by the chemist of the Department of 290 different specimens of corn: AVERAGE COMPOSITION OF AMERICAN CORN. Locality Dakota , New York Illinois Minnesota Nebraska Colorado California America, 1883 Albuminoids. Nitrogen. 10.75 1.72 10.54 1.69 10.06 1.61 10.07 1.61 10.47 1.68 9.89 1.58 10.26 1.64 10.31 1.65 There seem to be in Dakota, the right composition of soil and the proper tempering of the climate necessary to grow farm products of ex- treme richness. Mr. Clifford Richardson, chemist of the U. S. Department of Agricul- ture, report for 1885, says that the result of several years of scientific and (4) 98 KESOUKCES OF DAKOTA. chemical study leads to the conclusion that the yield of corn in the South is far inferior to that of the North, that a warm climate and a long period of growth, while producing a large kernel, tends to give a gross plant with but few ears and that while the size of the kernel of corn grown in the South is twice as large as that grown in the North — the yield per acre is less. Prof. Witcher, of the New Hampshire State College, asserts that fifteen tons of fodder of Northern varieties, will equal twenty -five tons of the Southern varieties of field corn, in nutriment. Corn planted on freshly broken sod invariably yields a fair crop, with- out cultivation. Sod corn is usually planted by dropping the seed in the furrow when breaking, and covering by turning the next furrow over it, or, with a sod hand planter between the furrows, after the breaking is finished. Sod planted in this way frequently produces twenty-five to thirty bushels of good corn to the acre. Corn on old ground is planted during the months of April and May, is never hoed, but is cultivated several times during the season with a sulky cultivator. The dent or flint varieties are found to do the best, and yields of from sixty to one hundred bushels to the acre have been reported. In many of the older counties corn is the chief farm product, fields of which, hundreds of acres in extent, are seen on every hand, and reports of yields, this season, of as'high as 100 bushels to the acre are common. With corn an assured crop, the raising of hogs has become an important and profitable branch of farming in Dakota. Alrtady several of the large cities have extensive pork-packing establishments in operation, and another season will see a large increase in the number of these institu- tions. If one-third of the land in Dakota, (33,000,000 acres) was sown to wheat and raised fourteen bushels to the acre, it would result in a crop of 4G2,- 000,000 bushels, — or more than the entire yield of the United States for 1886. RESOURCES OF DAKOTA. 99 FLAX. The culture of flax iu Dakota is barely in its infancy as compared with the interest that will be devoted to this crop in the future — when capital shall have built up within the Territory, manufactories to utilize the seed and the fibre. At present, owing to a lack of such industries, it is grown principally for the seed, and the fibre or straw is burned or wasted. Flax and sod corn are usually the first crops raised on new land. They can be sown on the freshly turned sod with a reasonable assurance of a good yield under any circumstances. Flax is one of the best subduers that can be grown on the sod, and places the ground in excellent condi- tion for working the next season, for any kind of a crop. Planted in this way it yields, ordinarily, from seven to fifteen bushels per acre, and in many instances, a single crop has paid for the land, in ad- dition to the cost of breaking and planting. Flax does exceedingly well on old ground, and one great advantage of the crop is that it can be put in late in the season — as late as the latter part of June — after the crowding work of the spring is out of the way. The culture of flax, to any extent, is confined to the district south of the Northern Pacific railway, and the larger crops are reported from the counties of the southern and central portions of the Territory. Even there, it seems to be confined to distinct localities; farmers in some com- munities running almost entirely to flax, while in others they show a de- cided aversion to having anything to do wuth it. The flax crop of the Territory in 1879, amounted to 26,757 bushels; in 1884, to 2,282,788 bushels; in 1885, to 2,916,983 bushels, and in 1886 to 3,844,323 bushels. From careful estimates based on a large number of reports, represent- ing every county, the acreage sown to flax in the Territory this season was 412,741 acres, and the yield amounted to 3,910,944 bushels, or an average yield of over nine bushels to the acre. Efforts are being put forth by many cities within the flax area, to build up flax mills, paper and cordage manufactories — efforts which are bound to succeed sooner or later, because of the great profit that would ensue to the farmer in raising the crop, could he find a market at home for the seed and straw, and because of the success awaiting the manufacturer, who will fill the demand already existing in the Territory for such products as 100 RESOURCES OF DAKOTA. are manufactured from, flax seed and flax straw. For the immense quan- tities of linseed oil, paints, oil-cake, straw-paper, cloth, twine, (especially that which is used for saving the wheat crop,) and other articles manufac- tured from flax, annually consumed in Dakota, we now pay a tribute to farmers and manufacturers abroad, which is justly due the people of our Territory. The introduction of flax mills will add a new source of wealth to Dakota, and furnish a wonderful impetus to the growing, by our farmers, of one of the most profitable crops. As has been said, flax is grown in Dakota solely, we might say, for the seed, while in Ireland, the plant is raised for the fibre, from which the famous Irish linen and other fabrics are made. Our method of threshing breaks up the fibre and renders it useless. This office has received a letter from San Francisco, describing a ma- chine, the use of which for threshing flax will not only secure the seed but also save the straw uninjured, a matter it would be well for our flax growers to consider. The manufacturer says that in his machine " the bundle of flax is dropped in the thresher where it is stripped of its seed bolls, the seed delivered clean in sacks, and the sheaf conveyed from the machine with the straw uninjured, and in condition to be used for textile purposes." It is to be hoped that some of our enterprising citizens will investigate the adaptability of the new machine to saving the fibre of the flax cron of Dakota, and thus render valuable a product which is now dis- carded by the farmers. The raising of flax has caused the building of numerous oil mills in the states of Minnesota and Iowa, — there being a dozen or more in Iowa alone. One of the largest oil mills in the United States, is located at Sioux City, and is supplied, to a great extent, with flax grown in-southeastern Dakota. It finds a ready market for all the oil and oil-cake it can make — the sales of its product being limited only by the capacity of the mill. The carrying out of the plans already undertaken for the building of a number of mills and manufactories in various parts of the Territory, will insure a home consumption of the farmers' crop of flax. Tow-mills haTe been established at the following points, viz. : Scotland, Brookings, Madison, Wentworth, Canton, Egan, and Vilas. The past season has been a profitable one for the manufacturers of flax-tow, and the few tow-mills now in operation have met with great success. The price of straw ran so high as four dollars per ton — with a great scarcity at that price. Some of the mills were compelled to shut down early because of the exhaustion of the supply of straw in their vicinity. The establishments for the manufacture of tow will be more than doubled before the close of another year. It is claimed that this soil gives the fibre of the flax a superiority over that raised in other sections. Yankton has a linseed oil mill, and another is talked of at Scotland, Bon Homme county. A paint manufactory is in operation at AVatertown, Codington county. RESOURCES OF DAKOTA. 101 OATS, RYE, BARLEY, .AND BUCKWHEAT. These grains are cultivated throughout the Territory with great success, and attain a size and solidity of berry elsewhere unknown. The adapta- tion of the soil and climate to the growing of these, as of all cereals, is manifested in the perfection of the grain and the large yield of the crops. This is especially true of oats, which returns a yield ranging from sixty to ninety bushels, weighing from forty to forty-four pounds. This office has a report, in one instance, of the extraordinary yield of 115 bushels to the acre. Rye returns a good yield, averaging from thirty-five to fifty bushels per acre, and weighing fifty-six to sixty-two pounds to the bushel. The berry is unusually hard, full and heavy. RYE CROP. Bushels. I860 1 70,) 1880 BHSi 24,359 i8S5 m US 196.750 1887 ^■■BHBH^HBBgHl 316,586 Barley yields from thirty-eight to forty-eight bushels to the acre, weigh- ing from forty-five to fifty-four pounds to the bushel. BARLEY CROP. Bushels. I860 1870 1 4,118 J 880 n 277,424 no oo /. oo 1. ■ 2,170,0.i9 The following tables exhibit the yield of oats and buckwheat for a num- ber of years: OATS CROP. Bushels. I860 1 2.540 18,0 H9B 114,327 ISM) ■ 2,217,132 1885 ■ m 22,970,098 102 RESOURCES OF DAKOTA. BUCKWHEAT CROP. Bushels. I860 1 115 1870 ■ 179 1880 ^■H 2,521 1885 IS 51,466 97,230 The acreage and yield of these crops, for the season of 1887, is ascer- tained from assessors' reports and other sources, to have been'as follows: Acres. Bushels. Oats Rye... Barley Buckwheat 1,172,289 43,267,478 17,559 316,586 235,155 6,400,568 5,749 97,230 Do not hesitate to write to this office for an answer to any question you may desire to ask about Dakota. If the pamphlets mailed you do not contain a reply to all your inquiries, or, if you are still in doubt about the climate, the productiveness of the soil, the rainfall, the vacant lands, or anything else upon which hinges your move Westward, write to the Com- missioner of Immigration, Pierre, Dakota, and your letter will be cheer- fully answered. RESOURCES OF DAKOTA. 103 TABLE SHOWING THE OATS CROP OF DAKOTA IN 1886, Iu comparison with each statu and territory of the Union. Rank. istaiLi. 45 WYOMING, 44 RHODE ISLAND, 4:> NEVADA. 42 LOUISIANA, 86,000 184,000 250,000 361,000 41 4C[ 39_ 3JT 37 36~ 35^ 34_ 3Y 32 3~f oO 29~ 38~ 2b 25_ 34_ 23 FLORIDA. DELAWARE, NEW MEXICO, MASSACHUSETTS, UTAH. IDAHO, NEW HAMPSH1 CONNECTICUT, COLORADO, MONTANA, CALIFORNIA. MARYLAND, MAINE. WEST VIRGINIA, WASHINGTON TER.. MISSISSIPPI, SOUTH CAROL! NEW JERSEY VERMONT, A LA ISAM A ARKANSA! 489,000 492,000 528,000 738,000 858,000 1,078, 0^0 1,081.000 1,123,000 1,591,000 1,987,000 3,317,000 2,470,000 2,701*000 2,803.000 3, 126, 000 4,749.000 5,102,000 5,301,000 6,276,000 7.9:39.000 s. 577, 000 10,219.000 11,369,000 18,521.000 20,651,000 21,865,000 25,516,090 30,577,000 31,798.000 317850,000 37,759. 000 656, 000 40 223.000 40,735,000 -.S 454 000 1 03,649 000 104 RESOURCES OF DAKOTA. VEGETABLES. The quality and quantity of the yield of vegetables of all kinds, grown in Dakota, cannot be excelled in any portion of the United States. Pota- toes grow very large in size, a single potato sometimes weighing as much as six pounds, are uniformally sound, very mealy and conceded to equal those grown in Colorado or any of the states of the Union. They yield from 150 to 500 bushels per acre. Onions are a prolific and sure crop, growing to an enormous size, and yield from 400 to 800 bushels per acre. Turnips, peas, beets, beans, parsnips, carrots, squash, Cabbage, cauli- flower, egg-plant, lettuce, radishes, melons, and all the field and garden vegetables are raised without more than the usual effort. All kinds of root-crops do well on sod, especially turnips and rutabagas. Turnips are usually sown in May or June ; rutabagas may be sown as late as July and will produce a good crop. For stock the mangel-wurzel is a very profitable root crop, is an enor- mous yielder and can be raised as easily as rutabagas. There never has been a season in Dakota when the crop of vegetables surpassed in yield or quality the growth of this year (1887). Potatoes,, cabbage, beets, squash, turnips, in fact everything in the vegetable line,, have yielded in a manner to surprise even those accustomed to the re- markable, from this prolific soil. Visitors to the annual Territorial Fairs at Grand Forks and Mitchell were astonished, more perhaps, at the dis- play of mammoth vegetables, than at any other exhibit. Here one found cabbage, each head of which weighed from thirty to forty pounds; squash, as large as giant pumpkins, and these latter (numpkins) weighing over 200 pounds ; potatoes, a half dozen of which would fill a half-bushel meas- ure; beets six inches in diameter and three feet and more in length and so on through the list. The potato crop of this season is one of the best ever gathered. The yield is large and the quality unexcelled. For the first time almost in the history of the Territory there will be a very large surplus for exportation KESOUKCES OF DAKOTA. 1C5 — and car-load shipments are now being made where, before, the crop has been insufficient for home demand. POTATO CROP. Bus/u'/s. 18(50 | 9,489 1870 m J 50,177 18S0_^ HBpHi 664,086 1885 W B m m ^^ SSImsaBsmsB 3,868,860 The figures for 1886 and 1887, if available, would show the same aston- ishing ratio of an increased product for the past two seasons as occurred be- tween the years of 1880 and 1885, the potato crop of 1885 being nearly six times larger than that of 1880; but a complete record of the crop statistics of the Territory for 1886 and 1887 is not obtainable, as much as the fact is to be regretted. The United States census returns for the years 1860, 1870 and 1880 fur- nish reliable information regarding the crops of the Territory for the seasons preceding those dates, and a census of Dakota taken in 1885, with all the safeguards against fraud which any Federal census possesses, shows the yield of the different crops for 1884. For the leading cereals, such as corn, wheat, oats, etc., the annual reports of the Department of Agricul- ture, Washington, have been taken as giving the only attainable estimates for the years since the Territorial census of 1885. The crop estimates for 1887, where given, are compiled from several hundred reports of farmers, merchants and reliable citizens, represent- ing each county of the Territory. The acreage and yield were reported by counties, there being several estimates in each instance for the same county, and the figures adopted by this office were obtained by striking an average of these different reports. This result was still further veri- fied by a comparison with the assessors' returns for the year — wherever they had been furnished. It is believed that the estimates of the acre- age and yield of the crops of 1887, as published in the preceding pages, are reliable and accurate. The comparative statements of the preceding pages, showing the enor- mous increase in the yield and value of the farm products of Dakota, during the short period of her settlement, are extremely interesting, and a most convincing proof of her certain supremacy among the agricultural districts of the Nation. 106 RESOURCES OF DAKOTA. HOPS. Hops of a superior quality grow wild along the James and Missouri rivers and on the low lands of the Black Hills, and yield a large and regu- lar crop. Prof. Walter P. Jenney, (U. S. geological survey, Black Hills,) in speak- ing of the fertility of the soil, says: " Wild hops attain a rank and luxu- riant growth in the bottom lands along the streams, and the soil and cli- mate seem to be remarkably well suited to the growth of this plant." There is certainly no reason why the growing of hops should not be- come an important industry in Dakota. The territory of the United States where hops are successfully grown, is very limited. A district in New York, for a radius of about forty miles, with Cooperstown, Otsego county, as its center, forms more than one- half of such territory, east of the Rockies; the only other places being three of the northwestern counties of New York, small portions of Ver- mont and Michigan, and parts of Wisconsin. On the Pacific coast the production of hops has increased from 15,000 bales, in 1880, to 70,000 bales in 1881. The fact of hops of good quality growing wild along the streams of Da- kota, is an assurance that the climate and soil are peculiarly fitted for the production of this valuable crop. This, together with the knowledge of the fortunes made by the hop-growers of the East, should be sufficient inducement for our farmers to give their attention to the subject. The entire population of the United States, sixty million people, could be settled in Dakota and have an acre and a half of ground apiece for elbow room. RESOURCES OF DAKOTA. 107 TIMOTHY, ALFALFA, BLUE-GRASS, ETC. The native grasses of Dakota are yet abundant and nutritious, and the mass of farmers depend almost entirely on prairie hay for forage for stock. But the time may come when the supply of wild hay will prove insuffi- cient, and it is well to inquire whether the tame grasses can be grown on Dakota soil. Dr. C. E. Bessey, of the University of Nebraska, in a recent communi- cation to the Prairie Farmer, furnishes pome interesting remarks in regard to the cultivation on the Western plains, of clover, timothy, alfalfa and other forage plants. He says: "Not only on the prairies, but away up the great slope of the plains, are the old grasses and clovers grown, and grown with great success and profit. Away up under the 100th meridian, timothy is now grown with excellent success. No one need question whether timothy is adaDted to the plains. Upon the lower plains it will grow to as great a size as upon the meadows of the Eastern farms. Upon the prairies wherever the soil is moist, red-top may be successfully grown. " There is no doubt that upon the low lands bordering the principal streams, red-top will be extensively cultivated. " Contrary to the expectations of many a farmer from the East, expe- rience has shown the grass to be an excellent one for pasture in the coun- try west of the Mississippi river. Of course, no one should depend upon it for hay; no one should ask it to bring him a hay crop. Blue-grass is eminently a pasture grass, and for this, when in its perfection, it stands unrivaled. " Originally it was taken for granted that red clover would not do well upon the soil of the plains, and few trials to grow T it w r ere ever made. The experience of those who were bold enough to make a trial, has shown that red clover is as much at home upon the plains as upon any of the Eastern soils. There can no longer be any doubt as to the adaptability of red clover to the soil and climate of the plains. White clover, while not extensively sown purposely, is appearing in many parts of the region west of the Mississippi river, and even beyond the Missouri river. It 108 RESOURCES OF DAKOTA. appears to do fully as well upon the soil of the plains, and without doubt, it will eventually be found throughout the whole of the great plain region." Timothy is grown by many farmers of the Territory, and universally with success. A farmer says of his experience in growing timothy on Da- kota soil: " In the spring of 1884, I sowed about an acre of timothy on sod-break- ing, with wheat, sowing about twelve quarts of seed just before harrow- ing the last time. The grass came up that season and made a good growth , with the wheat. The season of 1885, the timothy grew to a good height, and I cut it with the binder and threshed it for seed. The season of 1886 was very dry, as all know, and I supposed my timothy was killed, but not so; this spring (1887), it was growing nicely. This was sown on ground that was never backset and has passed through the dryest season we have had. If timothy will stand such a test with the chance this has had, there is certainly no doubt of its doing well in Dakota wherever planted." Alfalfa is one of the most valuable of the forage plants and produces enormous crops. It has not been cultivated to any extent on the prairies and plains, excepting in California and those parts of the West contiguous to the Rocky mountains. It is a clover particularly well adapted to the soil and climate of Dakota, and a forage upon which hogs and stock will grow and put on flesh all summer, without grain. The plant sends out a long tap-root, striking deep into the soil in search of moisture. Dry weather in nowise affects its growth, and once firmly rooted it is impossi- ble for a drouth to kill this grass. A farmer in Brule county, Dakota, says he has tried planting alfalfa on Dakota soil and that it grows beyond all expectations. He reports hav- ing plucked on the 15th of April this season, a sprig of alfalfa with twenty- five full, unfolded leaves and five inches high. " For an experiment," says a Richland county stock-grower, " I had an acre put down to alfalfa last year, seed put in the ground on the 15th of June, was cut twice and grazed down closely just before freezing up. The location is an exposed one, and the soil light and sandy; it has taken all of last season's and this spring's wind, and some of the young shoots this spring were buried fully six inches in sand. It could not have been given a harder test, even by taking especial pains to kill it out, and we have about one-half acre of it, of as rank, rich growth as could be wished for; the other half is thin and scattering, but may yet come forward in good shape, for, once well-rooted, I find it hard to kill. I intend giving it a second trial this season, and will put in about five acres more. We feel quite confident that we can grow it surely and profitably, on our sandy soil, and in doing so remove other obstacles in the way of cheap cattle production, i. e., the want of early and late green feed." A farmer of Pennington county, in the Black Hills, states that he has experimented, in a small way, with the growing of alfalfa, and with the most satisfactory results. The alfalfa has been cut four times during the season, yielding at the rate of eight tons of hay to the acre. RESOURCES OF DAKOTA. 109; Blue-grass lawns are quite common in the counties of sufficient age to have steadied down into efforts other than breaking the sod and the usual work attending the building up of a new country. There is not the least doubt that blue-grass will grow anywhere in Dakota, by exerting the care and attention required elsewhere to intro- duce this beautiful lawn grass; in fact, it may be said to grow with less effort, for ever since the year that General Custer camped at Yankton, in 1873, there has been a heavy growth of blue-grass on the old camp-ground. A great many of the Yankton people remove the sod and transplant it to their yards, where it thrives admirably. It is supposed Custer's com- mand carried baled blue-grass for forage, and the seed scattered in feed- ing the horses took root, and each year since, more seed has scattered, thus keeping up the supply. At Yankton, Elk Point, Sioux Falls, Fargo, Grand Forks and other cities of several years' growth, pretty lawns of rich-colored blue-grass are common. Hungarian and millet can be grown in Dakota with as little difficulty as attends the raising of these hay crops in the East. A Codington county farmer, last year, sowed thirty acres with Hunga- rian and millet, and raised 510 bushels of millet seed and 170 bushels of Hungarian seed. From this crop he sold $200 worth of hay, and fed at least thirty tons to his stock. He made more on the millet and Hungar- ian seed than on eighty acres of wheat. Following is the experience of a farmer in Flyde county with millet: " My first experience in Dakota with millet was in '84. Having half a bushel of seed, (the common kind,) that I brought from Michigan the year before, I concluded to try it on sod. Accordingly, I prepared the ground and sowed the seed the 20th of June. It being dry for a time afterward the stand was poor. I let it stand until ripe and cut it for seed, getting a little over two bushels from the whole. " The next year I sowed that seed over four and one-half acres of ground that had been plowed twice (beside the breaking). The ground was mellow and smooth, and the seed sown with the seeder, by shutting it off as tight as possible. In this way it sowed nearly one-half bushel very evenly over an acre. The seeder was followed by the planker, which left the ground smooth for the mower. "A heavy rain, a day or two after sowing, brought it up nicely, but three weeks of dry weather afterward stunted it some; but the heavy rains that followed through harvest of that year gave it a fine growth. This piece yielded twelve large loads of hay, besides fifty-six square rods of the piece being saved for seed, and which yielded twelve bushels of plump seed. Those twelve loads, with a few bushels of oats, fed the work- horses through the fall and kept the same through the winter, until March 1st, with no grain at all. They have never done better than they did on that ration. 110 RESOURCES OF DAKOTA. " It should be cut while in blow, or before, the seed is much more than formed, as the ripe seed seems to have a bad effect, if too much is eaten at once. It requires considerable time to cure, as it is so green and heavy when cut. It will do well if put into large cocks, after being sufficiently dried in the winrow, and let stand a few days. "It is easily damaged by rain, and should be well put up and well stacked. The time for sowing is any time in June, though it may be sown earlier or later and do well. It needs warm, moist weather to do its best. " From three pecks to a bushel of seed per acre is about right for hay, and half a bushel for seed. " The German millet is highly recommended as being large and yield- ing more than the common kind, but is coarser and needs to be sown very thick." Many farmers believe millet and Hungarian a more profitable crop than timothy. NATIVE HAY. The prairie hay crop in Dakota is a voluntary contribution of wealth by nature almost equaling in value, that of the cultivated farm products. A large yield of native hay, of excellent quality can always be depended upon. There never has been in the history of the Territory a complete disappointment ef the annual profits to the farmer and stock grower, de- rived from this crop, although during some seasons, the growth of the prairie grasses may be heavier and ranker, and the number of tons of hay gathered from an acre of ground, more, than others. This season the native hay crop is one of the best ever secured by the farmer and the amount in the stack is perhaps double that of the crop of last year. An unusual activity was displayed by our farmers in hay-making, because of the well known shortage of the crop in neighboring states — and thou- sands of tons have been harvested for export. There is a number of counties where the wealth flowing in from the sale of wild hay for shipment, a crop requiring only the labor of cutting and stacking, will bear no mean proportion to the amount received from products necessi- tating a season's toil accompanied by all the doubts and uncertainties of the farmer's vocation. Following is an exhibit of the hay crop (prairie hay) of the Territory for four seasons: HAY CROP. Tons. 18607" ■ "855 1870 1 527,987 The hay crop of 1887 will exceed 2,500,000 tons. KESOUKCES OF DAKOTA. Ill SORGHUM— SUGAR BEETS. The amount of sugar annually imported, and consumed in the United States and the tax paid by our citizens in the way of a protective tariff on this commodity is a revelation to those who have never investigated the subject. The value of the sugar and molasses imported into America last year, was $76,746,461, or, a little less than one-fifth of the entire dutiable imports of 18S6; exceeding in value, by almost double that of any other protected article of commerce. America paid out for duty on last year's imports of sugar and molasses 851,778,948, while the duty on all our im- ports of wool, and manufactures of, amounted to only $32,000,000; on iron and steel, and manufactures of, §14,600,000, and on silk, but 114,000,000. This fact is the more startling when it is known that every dollar of the sum annually sent abroad, for the purchase of sugar, which in 1886 amounted to 876,746,461, and of this indirect tax, making a total of $128,- 525,409 should be distributed among our farmers and manufacturers at home . The manufacture of sugar from the sugar beet has for many years been a leading industry of France — while in America with millions of acres of cheap land especially adapted to the growing of this tuber, farmer and manufacturer, both, have given but little attention to so great an oppor- tunity for amassiag wealth. Sugar is an article of necessity for which there will always be a constant and certain demand. This one article of food supply is costing us, in cash paid to other nations and in duty charges, a sum equivalent to one-half the value of the entire wheat crop of the Union. Here then is an opening for our farmers, for our enter- prising citizens, which will insure a return of wealth far exceeding in profit that of any industry now engaging their attention. There is no crop grown on the soil of Dakota with more certainty of prolific yields than vegetables, — especially beets. With proper investiga- tion, study and effort, our farmers could be brought to rival those of Europe as regards the production of sugar beets, and the entire sugar supply of America furnished by the manufactories of Dakota. Then there is the sorghum industry. The soil and climate of the Ter- 112 RESOURCES OF DAKOTA. ritory unite in the most favorable of conditions for the raising of sorghum. This is not a theoretical statement, but a fact demonstrated by the large yields, each season, of cane of a most excellent quality, although the area sown has been small and the product utilized — the juice or syrup only. That sorghum can be profitably employed in the manufacturing of sugar there is no longer the least doubt. During the past few years the industry has been carried on at two or more points in Kansas, under the supervision and control of the United States Department of Agriculture, and Commissioner Coleman has recently published an official statement declaring in positive terms the success of the undertaking. The Commissioner says: "The addition to the agricultural wealth and resources of Kansas will be enormous. The establishment of the sugar interest in Kansas gives a market value of $2 a ton to sorghum cane, a plant that grows in Kansas almost without care and with quite as much certainty as grass. At Fort Scott we talked with the cane growers unload- ing at the factory. One man had sold from fifteen acres 200 tons of orange cane for $400. From eighteen acres he had sold 231 tons of amber cane for $462. This was nearly fourteen tons to the acre, but taking twelve tons to the acre as the average, and this is $24, or equivalent at the average price of corn in Kansas to seventy-two bushels of corn, involv- ing twice the labor that is required to raise an acre of sorghum. Any farmer can make figures on this basis." "To every ton of cane, aside from the sugar in it, there are some ten or twelve gallons of molasses, and also the seed raised upon the cane, amounting to 25 bushels per acre, which is just as good for feeding all kinds of stock as Indian corn." This is an industry which should demand the immediate attention of the farmers of Dakota. Our soil will produce from twelve to fifteen tons of sorghum to the acre, yielding a hundred pounds of sugar to the ton of cane, and, used in this w r ay, Commissioner Coleman extends a profit to the farmer of $6 per ton, or say, $90 to the acre. RESOURCES OF DAKOTA. 113 FRUIT CULTURE. Long ago in those sections of the Territory, around Yankton, Vermil- lion, Sioux Falls, Canton, Scotland, and other localities where farming operations are a matter of some age, the question of raising fruit was set- tled satisfactorily, and during the past three years the conviction has be- gun to dawn on the minds of the people living in the newer counties further north, that the lack of fruit trees and shrubs growing about the farm yard, was the result of their own neglect and want of faith, rather than because of any difficulties attending the propagation of fruit on the prairies. At first, a few planted fruit trees as an experiment; wherever the trees were well cared for, a good, bearing orchard was the result, and served as a convincing argument to doubting neighbors. An unusually large number of fruit trees have been planted within the past two years. Each succeeding year will witness an increasing interest in the raising of home-grown fruits, and a widening of the area now sup- posed to be adapted to fruit- culture. Wild fruits, such as plums, grapes, choke-cherries, buffalo-berries, grow in abundance along the banks, and cover the islands of the Missouri and other streams. These wild shrubs bear in profusion a delicious fruit, plump and of good size, which is eagerly sought for by the house-wives for canning and preserving. Experiments made in cultivating these wild varieties have succeeded well. In the Black Hills there is an abundance of wild fruits of great, variety. Prof. Jenney, who visited this region in 1875, under authority of the Secretary of the Interior, to report on its cli- mate and resources, says: "The fruits found growing wild in the Black Hills are an evidence of the adaptability of the country for raising the more valuable cultivated varieties, and hence I propose to consider the wild fruits which are found in this region much more in detail than they would otherwise deserve. The most useful is the red raspberry, which was found in large patches in the vicinity of Terry Peak, at an elevation of 6,500 feet above the sea. The plant is rather dwarfish in size, the bearing canes being about two feet high, and August 15th, were loaded with deli- 114 RESOURCES OF DAKOTA. cious fruit, resembling very closely the cultivated variety 'Knerit's giant' in size, flavor and productiveness. A variety of black gooseberry was abundant on the western side of the Hills. The fruit was of a pleas- ant acid flavor, and of good size, only differing from the ordinary Western wild gooseberry in being blue-black in color, instead of dark red. Sev- eral species of currants, including the black, red, and fetid varieties were occasionally seen, but are valueless. The wild, Western strawberry grows throughout the Hills. It is a very shy bearer, and the fruit is deficient in flavor. The bunchberry or cornel (cornus Canadensis), was found in the extreme northern part of the Hills. I have never seen it elsewhere, ex- cept in Maine and Nova Scotia. Service berries (amelanchier Canaden- sis), were quite plenty on Spring and Rapid creeks, in July. The com- mon wild, red plum grows in patches among the foot hills along the bot- toms of the ravines. The fruit was ripe about September 20th. The only variety of grape noticed was a kind of frost grape, found along the banks of the streams, near the edge of the plains. Quite extensive patches of the two varieties of hazel nuts were observed in the southeastern part of the Hills, associated with alder, white birch, iron-wood, white-elm, burr- oak, sumac, the poison ivy, the Virginia creeper, and many other plants of wide range and distribution." The fact of fruits of such a variety, and bearing profusely, growing in all parts of the Territory, is of itself a sufficient guarantee of the adaptability of our climate and soil to fruit culture; but in addition to this, the success attending the efforts of a great number of farmers who have surrounded their prairie homes with bearing orchards, shows that fruit culture in Da- kota has passed the experimental stage, and the farmer who is without a supply of home grown fruit, has but himself to blame. A few statements are added, made by farmers who speak from experi- ence in the raising of fruit in the Territory. Yankton cunty — " At our last fair, ninety-two samples of apples grown in Dakota were exhibited, together with a fine display of grapes and plums. Small fruits of all kinds are raised without difficulty, and of ex- cellent quality." Turner count}' — " Two miles south of Hurley, there is a quarter section of land covered with fruit trees, vines and shrubbery, all growing, and much of it ladened with fruit. It would be hard to tell how many bushels of fruit of different kinds will be harvested. It would surprise anyone not acquainted with the fact to visit the place, and it is a sight well worth any person's time and expense, who cares to raise fruit." Lincoln county — " If anyone says that fruit cannot be raised in Dakota, he had better retract the assertion. Gus Lindeman, who lives about four miles south of Canton, raised such an enormous crop of apples last season, that he was compelled to prop up the heavily ladened limbs for fear they would break off. There were several farmers in Lincoln county who had apples all winter, that were raised on their own soil and planted bv their own hands." RESOURCES OF DAKOTA. Bon Homme county — " If any person has doubts about this being a fruit country, he is invited to call at this office and inspect a small branch from one of Mayor Stafford's Siberian crab-apple trees, and have his doubts dis- pelled. The branch contains upwards of sixty perfect apples, and is a fair sample of the trees in the mayor's garden." Kingsbury county — " Mr. A. M. Barker, who has had a good deal of ex- perience in fruit growing savs, that he never had as good success in rais- ing apple trees anywhere else as he has had in Dakota. The trees do not blight or winter-kill, and make a rapid growth. M. Pearce — " My success, and that of others for the last few years, con- vinces me that with the right varieties, properlv taken care of, there are no crops so valuable as the small fruits; but each must be taken care of; none of them will bear neglect. All require good soil, such as would pro- duce a good crop of corn, and plowed deep and harrowed level. Plant in the spring when the ground gets warm, — say about the 10th of May." Burleigh county — "Most kinds of garden shrubbery thrive, and fruit bet- ter here than in the states. One need only make a trip to the fruit farm of Mr. John Millet, four miles north of Bismarck, to be thoroughly con- vinced of the fact. The visitor can see gooseberries, currants, raspber- ries and blackberries growing in full vigor. The canes and shrubbery were last season so loaded with fruit that they bent to the ground." Minnehaha county — " Strawberries, raspberries, currants, and all kinds of small fruit are raised here in great abundance, and of unsurpassed quality. Orchards have been established which are astounding even their owners by the yields that are secured, and by the evidence that this region will, in not many years, be as much noted for its apples, and large fruit generally, as it already is for its cereal products." Morton county — " A farmer who set out a few apple trees in this country, west of the Missouri river, as an experiment, a few years ago, has a good prospect for fine fruit this year, and is satisfied that nearly all fruits can be grown successfully here. The strawberries are fully up to those grown in the most favored locations of New Jersey, the strawberry paradise." Clay county — " In the matter of fruit especially, Clay county is pre-em- inently ahead of all other sections. An inspection of several orchards near Vermillion would be a cause of surprise even to a resident of one of the other counties who may think he himself has succeeded in fruit cul- ture. Apples, crabs, plums and grapes are to be found in great variety, and of healthful growth." At the last Territorial fair this (Clay) and Turner county had on exhibi- tion a display of fruit which would have been creditable to any state of the Union. The Clay county exhibit included thirty different varieties of apples alone. L. J. Moore, Richland county — " I have about fifty bearing apple trees besides numerous currant bushes and a large strawberry patch, all of which have done well considering the fact that I have left them to shift for themselves." 116 RESOURCES OF DAKOTA. Butte county — " While speaking of berries we will say, that strawberries, red raspberries, service berries, two kinds of buffalo berries, besides choke cherries and plums, grow luxuriantly in the Hills; we can see no reason why the farmers can not have all the berries they could use if they felt disposed to cultivate them." Pennington county — " Anyone who imagines that fruit cannot be suc- cessfully grown in this part of the country should visit the nursery of Hale and Thomson on Box Elder creek, five miles north from town, to have such impression removed. The nursery this season turned out several thousands of quarts of strawberries, while the currant, gooseberry and raspberry bushes are heavily loaded. The- vineyard gives promise of a fine yield of grapes, the Concord variety showing up particularly well. Apple trees of a number of varieties will also yield well this year. As for shade and ornamental trees, there are many thousands of them ranging from seedlings to three-year-olds. And it must be remembered that this is a young nursery. What it will be in five years from the present time may possibly be guessed when the fine growth already made by the stock is known." Other counties make equally as good reports of the success attending fruit culture wherever tried. The Dakota Farmers' Alliance recommends the following varieties of fruit for Dakota: Apples — Wealthy, Duchess, Tetofsky; and in the Missouri valley as far west as Bon Homme county, Walbridge, Fameuse, and Haas. Hybrid apples: Whitney No. 20, Crab, Transcendent, and Hyslop. u Raspberries — Turner and Cuthbert; black raspberries, Gregg, and Doo- little. Strawberries — Crescent, and Downing. Currants — Victoria, Red Ditch, and White Grape. Gooseberries — Downing, and Houghton. Early Richmond is recom- mended for trial. Plums — De Soto, Forest, and Garden. Grapes — Worden, Janes ville, and Concord. The writer has a vivid recollection of assisting, some twenty years ago, in the planting of the first fruit trees ever grown in a county of a neigh- boring state. At that time it was thought fruit-culture could never suc- ceed so far West, and many were the comments volunteered as regards the folly of the venture. To-day, that little county makes return of more than a hundred thou- sand thrifty fruit trees, and in 1883 the value of the horticultural products for the state, amounted to $1,640,525. The man who is skeptical as regards the raising of fruit in Dakota will live to see the wonderful success which has attended the efforts of the early settlers there, repeated in our own grand Territory. The value of orchard and nursery products for 1880 in the Territory, RESOURCES OF DAKOTA. 117 amounted to $156; in 1884 the value had increased to $13,378— nearly 1,000 per cent, in four years. From 1884 to the present time, the ratio of increased investment in fruit culture is even greater, but reliable figures are not available. In many localities the farmers have organized societies to further the interests of horticulture and forestry, and, in addition, there is a Territo- rial organization, by name the " Dakota Horticultural and Forestry Asso- ciation," officered as below: President, E. DeBell, Sioux Falls; Vice President, G. H. Whitney, Es- mond; Secretary, Mrs. L. A. Alderman, Hurley; Treasurer, A. W. Hayes, Parker. The power which is to mould this Nation and the world lies in the West. — [Bishop Whipple. 118 RESOURCES OF DAKOTA. TIMBER. *The entire area of the Black Hills is a well wooded country. The density of the forests clothing the hill sides have, from their sombre hue when viewed from a distance, given the name to this region, the " Black Hills," by which it is known also in the Indian dialects. The following trees yield timber in this section: The heavy pine, (pinus ponderosa,) often known as yellow or Norway pine, the most abundant and valuable tree in the hills. Black and white spruce, found among the valleys in the central and northern portion of this region, covering a considerable area. Burr-oak, (quercus macrocarpa,) in small groves on the eastern slope, near the foothills. White elm, (ulmus Americana,) associated with the burr-oak, occurs along the valleys of the streams near the eastern and southeastern foot- hills. Aspen, white birch, ash, mulberry, box-elder, (negundo,) iron-wood, (horn beam,) and juniper, grow sparingly in different parts of the Hills, but are of little comparative value. The pine forests cover so extensive an area and yield so large a propor- tion of the timber, that all the other trees combined may be neglected in comparison, though they will be found valuable in the future develop- ment of the country. The Norway pine is a tall, straight tree, free from limbs for one-half its height from the ground. The wood is white, soft, with a straight, some- what coarse grain, free from knots and splitting readily into "shakes," shingles, or other similar forms. The sap is more resinous than that of the white pine, and, in this respect, this variety approaches more nearly the pitch pine of North Carolina, a tree which it somewhat resembles in its style of growth. On the bottom lands in the lower valley of French creek, specimens of this pine were seen that were fully 100 feet in height and would measure thirty-five to forty inches through at the ground. Trees of these large Prof. Jenney's report on the resources of the Black Hills. RESOURCES OF DAKOTA. 119 dimensions are, however, rare in the Hills. Timber of from twelve to twenty-four inches in diameter is common, while extensive tracts are covered by a dense forest of small, slender pines from fifty to sixty feet high, and rarely less than eight, or more than twelve inches through at the ground. The pine forests in the Black Hills, where the trees are of mature growth and uninjured by wind or fire, furnish good straight saw logs from thirty to fifty feet in length, and very uniform in thickness, with a gradual taper, averaging in diameter from twelve to twenty inches. * * * * On the elevated portion of the interior of the Hills, especially along the valleys in the limestone formation, extending from Custer Peak to Floral valley, and on the headwaters of Rapid, Castle, Elk, Bear, Butte, and Spearfish creeks, two varieties of spruce, resembling the black and white spruce of the Northern states, are quite abundant. The trees are tall, growing thickly together, and furnish logs quite uniform in diameter throughout their whole length. By careful measurements of the map, the area within the timber line, or outer boundary of the forest at the edge of the plains, is 3,800 square miles. One-half of this, or 1,900 square miles, is covered by woods, in- cluding the large forests of young trees, as well as the sections of valuable timber. I estimate that one-fifth of the above area of the Black Hills, or nearly 800 square miles, equal to 500,000 acres, is covered by timber of merchantable quality, suitable for cutting and sawing into lumber. This was the condition of the timber area of the Black Hills, when ceded by the Indians in 1876, and though the annual demand since, for mining timbers and for lumber, has been quite heavy, a large part of the forest is still remaining. It is estimated that each year in the Hills, more than twenty-five million feet of pine logs are manufactured into lumber — none of which is exported. Nearly the entire stock of lumber used is manufactured from the native forests. Along the Missouri river cottonwood, ash, willow, and box elder timber grows to a considerable extent, the groves occasionally widening to forests of some magnitude. The islands are invariably densely covered with trees and shrubs. Around Devils Lake there is a large belt of timber, and another much more extensive in the Turtle Mountains near the Canada line. The banks of the Red River are lined with oak and other forest trees of large size. Its tributaries the Sheyenne, Wild Rice, Maple, Goose, Turtle, Forest, Park, Tongue, and Pembina rivers are also well timbered. The course of the Mouse, is marked by a heavy growth of timber, such as oak, ash, aspen, box-elder and other varieties. On the coteaus between the Missouri and Jim rivers, and in the breaks of the hills west of the Missouri, patches of timber occur frequently. All of the streams emptying into the Missouri from the west, and many of the lakes scattered about the Territorv, are more or less timbered. The 120 RESOURCES OF DAKOTA. settler in the vicinity of any of the multitude of smaller rivers will find no difficulty in obtaining a plentiful supply of cheap fuel. Grand Forks, on the Red River, is a lumber manufacturing point of great importance. Two mills alone have a capacity of over 200,000 feet of pine lumber per day. The annual out-put of lumber of the mills of Grand F'orks is estimated at 20,000,000 feet. The logs are rafted down the Red from the pineries of Minnesota. Hon. Lauren Dunlap, lately in charge of this office, in writing of the na- tive timber has said : "While it may be news to some people to learn that Da- kota has such a timber acreage even as reported, it is nevertheless a fact, that the total timbered area, native and cultivated, in Dakota, considered in one body, exceeds at this time the area of each of several Eastern states. There are more acres of native timber in the Black Hills alone, than in either Rhode Island or Delaware." Remember that this office answers every inquiry, no matter how trivial, coming from anv one interested in Dakota's growth and advancement. RESOURCES 0* DAKOTA. 121 CULTIVATED TREES. Science has demonstrated that the growth of trees has an effect on the meteorological conditions of any locality, of the highest importance. Any number of instances are recorded where the wholesale destruction of for- ests have changed the condition of localities from that of gardens of fer- tility to something a little better than a desert waste, and, vice-versa, where the re-foresting of a denuded country has led to the most beneficial results as regards the climate, the precipitation of moisture, the atmos- pheric currents and the temperature of the atmosphere. The Chief of the Bureau of Forestry in a report to the Commissioner of Agriculture, cites the remarkable instance of the island of Ascension, which was entirely barren when first occupied in 1815, and so destitute of water that supplies were brought from England and the Cape of Good Hope. Means have since been taken to plant trees and to introduce ag- riculture on the island. The effect has been remarkable. The island grows forty kinds of trees, where but one grew in 1843, owing to the want of water. The water supply is excellent, and the garrison and ships are now supplied in abundance with vegetables of various kinds raised on the island. And of the island of Cyprus, once regarded as one of the richest and most fruitful islands of the Mediterranean, which, when it fell under the power of the Turks, was stripped of its woods with the most baleful effects. The rainfall diminished, water courses dried up, swamps formed on the sea shore and the island was visited by deadly malaria. On falling into the hands of Great Britain, one of the first duties of the British gov- ernor was to see to the preservation of the few remaining patches of forest, and to plant hundreds of thousands of blue gum trees in the low swampy lands of the coast, with the view of neutralizing the malarial ex- halations from the soil. These plantations are only five years old, but they are said to be exercising, already, a very beneficial result. The Encyclopedia Britannica ascribes the political decadence of Spain in a great measure to the destruction of its forests, and remarks that the evils of denudation are perhaps nowhere more signally exemplified than in Spain. 122 RESOURCES OF DAKOTA. And Sicily, once the great grain reservoir for Rome, after the island was despoiled of its forests gradually lost her fertility and mildness of climate. The ruins of proud and opulent Syracuse are in a desert covered by sand, which the hot sirocco carried over the Mediterranean sea from Africa. A few isolated, well watered and carefully cultivated districts of very limited extension, is all that is left to remind the tourist of the by-gone glory of Sicily. Similar examples of the great evils following the obliteration of forest, and of the benefits resulting from re-foresting, are to be found in the his- tory of nearly all of Europe. It has been so in Germany, in France, in Herzegovina, in Montenegro, in Italy, and with the islands of Ceylon, St. Helena, Santa Cruz, and Ternate. And such instances are not wanting even at home, though the period of settlement is but a day in comparison with that of Europe, and the con- sequent destruction to the forest though rapidly going on, is not yet fully completed. No country on the face of the earth possessed the magnificent forested do- main equal to that of the United States Government when first estab- lished, but a hundred years of spoliation and waste, in addition to legiti- mate sale and . transfer, are rapidly doing the work of depletion. The entire forest area of the United States is estimated to be less than 450 million acres, of which the Government owns eighty-five millions. It is estimated that the annual consumption of timber in the United States amounts to twenty billion cubic feet. Hon. Emil Rothe, before the American Forestry Congress said: " Have you never tried to find out why southern Ohio has ceased to be the great fruit country it was formerly known to be ? Why is it that we cannot raise any more peaches in our state, while they used to bring sure crops not more than a quarter of a century ago? What is it that makes our climate once so favorable to mankind and vegetation, more unsteady from year to year? Look at the woodless hills of southern Ohio and you have the an- swer. Let the hills be deprived of the rest of the protection which the forests afford, and half of the area of the state will be sterile in less than fifty years." Hon. Cassius M. Clay, of Kentucky, said on the same occasion: "I move in the sphere of experience with more certainty. I remember when the forests were hardly broken here, that springs of water were very frequent and perennial. The rivulets, creeks and rivers had a per- petual flow. These have now changed. The rivulets and creeks are now dried up in summer, and the fish so often caught by me in earlier years are gone. Not one spring in a thousand remains. Indian corn was gen- erally planted in March, and the rains and exhalations of moisture from the surroundings made crops successful every year. Now, the destruction of the forests has lost to us that bed of leaves which was a perpetual res- ervoir of water for springs and evaporation; aided by the treading of the RESOURCES OF DAKOTA. 123 hard surface, the rainfall, if the same as of old, rushes off at once, sweep- ing the soil into the Mississippi delta. Dry winds absorb not only the ancient humidity of the air, but drink up the sub-soil evaporation, so that our winters are longer, more changeable and unendurable. Corn can hardly be safely planted till late in April, and drouth too often ruins all, in spite of our best efforts." The more one investigates the subject, the more convinced he must be- come tnat the planting of trees has a decided effect upon the regulation of storms, the formation of clouds and the descent of rain. It has been esti- mated that the leaves of a single tree, of large growth, would cover an area of more than 200,000 square feet, and that they give out every fair day of the growing season, 15,500 pounds, or seven and three-fourths tons of mois- ture. Multiply this sum by tens of thousands, and can one longer doubt the result of the humidity of the atmosphere, following the cultivation of forests? How wise, then, was the policy adopted by Government of fostering and encouraging the planting of trees and forests on our own Western plains, and what a grave error is about to be committed in the repeal by Congress of the timber culture act ? There may have been an occasional fraud perpetrated against the Government in obtaining title to a portion of the public domain, under the provisions of this law, but all laws, even the most useful, lead to evasions. No one who is familiar with the settle- ment of the Western plains, can gainsay the assertion that the enactment of the timber culture act was one of the most salutary laws ever passed by Congress, and has led to the growing of millions of trees and acres of for- ests upon the prairies of Kansas, Nebraska, and of Dakota, where otherwise would have remained an ocean's surface, unbroken by the pleasing sight of tree or shrub. That these forests planted in the West, have had a beneficial result in modifying the storms and increasing the rainfall, statistics of the National Weather Bureau give abundant proof. The good that would yet result to the prairies of the West from a con- tinuation of the law, guarded by such careful provisions as Congress may see fit to place around it, cannot be over-estimated. Hon. F. P. Baker, special agent of the U. S. Department of Agriculture, in speaking of the workings of the timber culture act in Kansas, says: " The passage of the timber culture act w r as one of the first steps taken by the Government in recognition of the necessity of tree-growing on our Western prairies. I have no hesitation in saying that the law has done a great deal directly, and much more indirectly, toward covering with forest trees great tracts which would otherwise have been left bare to be scorched by the sun, swept by the hot winds, thus to aid in perpet- uating the reign of drouth and grasshoppers in the Western country. Let any man visit the counties of Kansas, settled since the passage of the timber culture act, and he would see more trees growing than were to be 124 RESOURCES OF DAKOTA. seen in prairie counties settled before the passage of the act, and. within ten or fifteen years after their first settlement." As an example of what has been done in tree planting, Mr. Baker cites the states of Kansas and Nebraska. In the latter state it is estimated that there are growing 53,000,000 forest trees planted by the hand of man. It is safe to estimate the same number to the acre as is required under the timber culture act — that is 675. This would give a little over 78,000 acres in forest trees in that state. In Kansas, the statistics given by the report of the secretary of the State Board of Agriculture show 119,682 acres, and the same calculation as above would show the number of trees in artificial forests in the state to be 70,486,350. In Dakota 1,091 final proofs have been made to date, (June 30, 1887,) under the timber culture act and, as the law requires ten acres of healthy growing trees before the final proof will be accepted, we must have at least 10,910 acres of trees and calculating the legal requirement of 675 to the acre we have 7,364,250 growing trees on the prairies of Dakota as an accomplished result of this beneficial and wise act. But this is only a partial showing of what has been done in Dakota through the encourage- ment by Government of the planting of forests. It will be remembered that it requires eight years from the date of entry at least or as much as thirteen years if the full extent of the law is taken, before final proof can be offered on a timber culture tract. Therefore, timber culture entries made since 1879 are all incomplete, with a possible addition of many more made prior to that date by entry-men who have taken advantage of the longer term allowed by law. There are 52,226 of these entries and estimating that the law is being complied with since 1880 in the same ratio as the number of final proofs offered to date bear to the whole number of entries made up to 1879 — it would show 63,130 acres of growing forest or 42,612,750 trees in all, for which the citizens of this treeless region must bless the provis- ions of the timber culture law. In 1882 there were 4 final proofs made of timber culture in Dakota. " 1883 " " 111 " 1884 " " 169 " 1885 " ", 161 " 1886 " " 275 " 1887 " " 371 The timber culture act should not be repealed. Even in its present shape it is accomplishing as much good as any of the laws ever enacted by Congress governing the public domain. But, rather, so amend it that title to one-quarter of each section of land, remaining subject to entry, can only be obtained by a full compliance with the timber culture act, and at once you sweep away all danger of evasions and increase ten fold the benefits to accrue to the Nation by compelling an enlargement of the area devoted to forests. This subject has been dwelt on to a tiresome length because it is our desire to impress on the new-comer the many advantages of devot- ing some little attention to the propagation of trees. It not only beautifies KESOURCES OF DAKOTA. 125 the farm and home, but serves to break the force of storms and each tree planted adds its mite toward the gentle distribution of the rainfalls and the tempering of the searching winds. Not only that, but there is no ven- ture so profitable — and attended with so little risk as that of tree culture. Emil Rothe, in a lecture on the profits of forest culture, has said: " Many millions of dollars of American capital are invested in various enterprises which require a much longer time to yield profit or income and never pay nearly so well as systematic forest culture in the proper locality. There is certainly no risk in forest culture. It produces an article of general and steadily increasing demand, and it can be calculated with almost math- ematical certainty what profit may be derived from it and within what time. "The fact that it is highly remunerative in all Europe where land is much higher in price than here, should justify the expectation that it will be profitable. It is well known that on this continent forest trees grow much quicker and comparatively taller than in the Eastern Hemisphere. Here, the most useful trees attain their full development in two-thirds of the time required in Europe, an advantage which can hardly be over- estimated. "The governments of Prussia, of several of the smaller German princi- palities, and of France, Austria, and Italy make forest culture an unfailing source of a large yearly income. They find it profitable to buy tracts of inferior lands at prices equal to those of our best farming lands, and to stock them with timber. "Only the better class of wheat or meadow-land nets a greater average revenue, in twenty-five years, than well managed forests — a fact which may, at first sight, seem incredible, but which is easily accounted for Ly com- parison between the yearly expenses of grain culture and the trifling out- lay required for the planting and maintenance of a forest after the trees have become two or three years old, and by taking in consideration the frequent failures of grain crops and the sure steadiness of the growth of trees." By all means plant at least a few trees about your farm and do it at once. You will live to reap the reward of your efforts and forethought in a hundred different ways. There is not the least difficulty in growing trees anywhere on the prairies if proper care is taken in selecting the varieties and in the man- ner and time of planting them. Some exertion, too, must be expended for the first two or three years, in cultivating in and about the trees. Hon. N. H. Egleston, ex-chief of the Government Bureau of Forestry, says: "The prairies are destitute of trees, not on account of peculiarities of soil or climate, but -from other causes. AVe have ample evidence that they w r ere once clothed with an abundant arboreal growth, and these re- ports, with other facts, show that they may be covered again with such a growth, so far as it is for any reason desirable. In almost all portions of the prairie region, even those least favorable to vegetable products, on 126 RESOURCES OF DAKOTA. account of the deficiency of the water supply, groves and belts of trees of various kinds — the result of planting during the last few years — prove that with proper care in the cultivation of trees, and in guarding them from injury by lire or by roaming animals, forests may be established in sufficient abundance to meet all demands for lumber and fuel, and to se- cure those climatic and other influences on account of which forests are valuable to any country." In the report on Government forestry, 1884, forty-seven different kinds of trees were reported from Dakota as having been tried by planting. In order of preference the leading varieties are as follows: Cottonwood, box-elder, ash (white), walnut (black), maple (soft), elm (white), willow (white), oak, maple (hard), butternut, poplar (Lombardy),balm of Gilead, basswood (or linden). The following recommendations as regards tree planting are offered by- the Dakota Horticultural society: Trees for forest planting: box-elder, white or green ash, rock elm, larch, white birch, soft maple, butternut, cottonwood, black cherry. For wind breaks or shelter belts: white willow, cot- tonwood, box-elder. For street planting: white elm, hard or sugar maple, basswood, hackberry, ash. Ornamental planting: white birch, larch, bird cherry. Evergreens for forests planting: Scotch pine, red cedar, white pine, American arbor vitse, European larch, (conifer, but not an ever- green.) Ornamental evergreens: dwarf mountain pine, Colorado blue spruce, Northern white spruce, Siberian fir, red cedar, Scotch pine, Nor- way spruce, arbor- vitse in variety. This office has reports of a cottonwood tree twenty years old, recently cut down, which had attained a circumference of seventy-five inches, and when cut up furnished two and one-fourth cords of wood. Another report says that trees eight years old grown from seed are now fifteen feet high, and four inches in diameter. The Territory makes the following exemptions from taxation as a reward for tree planting: Any one-fourth part of any quarter section of prairie land, the same being a legal subdivision, on which five acres of timber shall be planted, either by sowing seed or by setting trees or cuttings, and the same to be kept in grow- ing order by cultivation, and not to be more than twelve feet apart each way, together with all improvements thereon, not to exceed in value $1,000, and for a period of ten years from and after the planting of said timber ; and any change of ownership of such land shall in no way effect the exemption from taxation as herein provided. All improvements made on real property by setting out either forest or ft ait trees, shrub- bery or vineyards, which shall not be considered as increasing the value of the land for purposes of taxation. Let us plant more trees, and who knows but that our millions of acres of growing forests will some day supply the inhabitants of the East with number— as well as our wheat fields will furnish them bread. KESOURCES OF DAKOTA. 127 The importance of forestry has been recognized for many years in other countries. In Germany the management of forests by the state has been carried on for hundreds of years. In Hanover there are 600,000 acres in the government forests, the annual expense of keeping which amounts to 1650,000, the receipts $1,500,000, and the profit $850,000. The state forests of Saxony cover nearly 400,000 acres, and yield a net yearly rental of $1,250,000. The state forests of Bavaria are even greater in extent, and return, after paying all expenses, $4,500,000 per annum. Austria, France, Russia, Sweden, Italy and Denmark, have schools of forestry maintained by the government, and the national forests are protected by stringent laws. In Sweden, even farther back than 1647, the party who cut down a tree was required by law to plant two in its place — a law it would be well for our Government to imitate now. For many years the United States did nothing to encourage forestry. The first timber culture act was passed by Congress March 3, 1873, and amended March 13, 1874. The passage of this act has strengthened the growing sentiment in favor of forestry, and led to the establishment, by the Federal Government, some five years ago, of a Division of Forestry, the present chief of the Division being Mr. B. E. Fernow. Many of the prairie states organized forestry associations, and encour- aged in other ways the planting of trees. Twenty-three states and territories recognize the importance of trees upon the prairies about the homes, along the streets, and in the public parks and school grounds, by designating a day, usually in April or May, termed an Arbor Day, which the people are urged to devote exclusively to the planting of trees. The governors of these states and territories designate the day by annnal proclamation, and request the closing of schools and all places of business, and that all manner of labor cease, in order that no citizen may be deterred from planting a tree. Arbor Day originated in Nebraska some fifteen years ago, under the ad- ministration of Governor Morton, and it is estimated that there are over 600,000 thrifty trees in that state, where,prior to this day devoted to arbor- eal production, there were scarcely any to be found except along the streams. The observance of Arbor Day in Dakota is said to owe its first sugges- tion to Rev. C. F. Clapp, formerly pastor of the Congregational Church, Yankton. In the spring of 1884 Mr. Clapp called the attention of Acting Governor Teller to the fact that many Western states had adopted such a custom and suggested that Mr. Teller issue a proclamation for the obser- vance of Arbor Day in Dakota. The Acting Governor agreed to Mr. Clapp's suggestion, issued his proclamation and the custom has been regularly observed during the three years since. The present execu- tive, Governor Louis K. Church, designated May 5, 1887, as Arbor Day, declaring the same a legal holiday and urged the people to devote it exclusively to tree planting. The day was very generally observed and 128 RESOURCES OF DAKOTA. thousands of trees were planted by the school children, the arboreal so- cieties, the village authorities and the individual citizen. This office has received reports of the day's celebration from every section of the Terri- tory. There were more trees planted on Arbor Day, this spring in the three towns alone, of Mitchell, Huron and Yankton, than were reported last year from the entire thirty-seven counties reporting. Owing to the dif- ference in climate in a territory of so vast an extent as Dakota, an Arbor Day cannot be designated suitable to all the varying conditions and many trees were planted prior and subsequent to the date named by the Gover- nor of which this office has received no reports. It is quite safe to estimate the trees planted this spring, (other than those planted under the timber culture act,) at upwards of a million; and the number planted the three years previous would certainly exceed a million and a half. This number, added to the trees planted under the timber culture act, shows a grand total of 44,112,750 cultivated trees in the Territory to-day, and, estimating the number to the acre as is required under this act — 675 — would give 65,352 acres of forest. The results of tree culture are plainly observed in the towns and around the farms, where age has worn off, somewhat, the excitement of business engagements and subdued the fever of real estate speculations. In the cities of Yankton, Elk Point, Sioux Falls, and other towns, and the country surrounding them — the old settled area of the Territory — the trees and shrubbery growing about the yards and along the streets and roads present as favorable a view to the visitor as is to be seen in cities of the East, where the trees are native. The towns and communities of youthful age are imitating with commenda- ble zeal the examples set by the older places, and within a few years the Dakota village or farm destitute of the shade and ornament furnished by trees, will be remarked as a noticeable exception. Our law-makers have wisely amended the general law governing the incorporation of cities in Dakota, so as to permit the city authorities to compel the planting of trees along the streets, by ordinance, in the same manner as sidewalks are constructed. This will insure a regularity of time, of distance, and of the variety, in the planting of shade trees; and place their care and protection in the hands of a public officer. With such a provision there will be no treeless spaces to mark the resi- dence of the unthrifty citizen or to point out the investments of Eastern speculators. RESOURCES OF DAKOTA. 129 STOCK RAISING. While the leading industry of Dakota is the tillage of the soil, the live stock interests are rapidly assuming a rank of equal importance with re- spect to the amount of capital invested and the revenue derived there- from. The census of 1880 gave the value of all farm products in Dakota for the crop year of 1879 at $5,048,814, while the value of live stock was placed at $6,463,274. In 1885 the products of the farm had increased to $36,808,131, and the value of live stock to $40,528,897. On January 1, 1887, the value of live stock in the Territory had reached the vast sum of $43,195,229 — an amount nearly 50 per cent, greater than the value of the three principal farm products, wheat, corn, and oats — of the same year. If we add to the sum given as the value of Dakota's live stock, the value of the dairy products and of the wool clip for the same year, some idea may be had of the rapidly increasing investment by our farmers in the growing of stock. VALUE OF LIVE STOCK. I860 I Dollars. 39,116 1870 H 779,952 1880 1885 BBBH E5 6,463,274 gU ~ 40,528,897 1887 Ell IMWM Will SH 43,195,229 In 1880 there were in the Territory 41,670 horses, 2,703 mules, 40,572 milch cows, 100,243 head of cattle, 30,244 sheep and 63,394 hogs. In 1880 these numbers had increased to 227,027 horses, 11,964 mules, 199,480 milch cows, 710,934 cattle, 256,209 sheep and 427,176 hogs. Official returns show the percentage of increase in the number of animals for the year ending January 1, 1887, as follows: Horses, 10 per cent. ; mules, 3 per cent. ; milch cows, 10 per cent. ; cattle, 13 per cent.; sheep, 1 per cent., and hogs 20 per cent. In seven years the value of live stock, in Dakota, has increased $36,- 365,064, or more than an average increase of $5,000,000 per year. (5) 130 RESOURCES OF DAKOTA. TABLE SHOWING THE NUMBER OP OXEN, MILCH COWS AND OTHER CATTLE In Dakota, 1886, and their value in comparison with each state and territory of the Union. BANK. STATES AND TER. NUMBER VALUE. DOLLARS. 47 RHODE ISLAND ! 35,810 1,236,531 46 DELAWAEE, I 55,820 1,597,762 45 CONNECTICUT, 1 234,586 7.638,973 44 NEW HAMPSHIRE, 1 236,933 7,216,412 43 NEW JERSEY, i 242.866 8.572,522 42 ARIZONA, ~I 258,942 4.985,853 41 UTAH, ■ 264.376 5,834,891 40 MARYLAND, ■ 273,262 7,412,891 39 MASSACHUSETTS, ■ 285,617 9,580,502 38 NEVADA, ■ 334,742 7,588,289 37 MAINE, n 351,009 10,101,379 36 SOUTH CAROLINA, ■ 361,606 4,955,850 35 WASHINGTON TER., 34 IDAHO, ~B~ 363,079 363,951 9.107,148 8,155,670 33 VERMONT, 399,705 10,884,624 RESOURCES OF DAKOTA. 131 The immense yield of the grain crops of Dakota has been heralded far and wide, and deservedly, too; yet we must not lose sight of the fact that the live stock interests have contributed a big share in building up the present wealth and prosperity of the Territory, and that each year is witnessing an astonishing increase of investment in this direction by the farmer. It is with a feeling of great satisfaction, and a conviction that the farmers of Dakota have discovered the sure road to success and wealth we observe this rapid enlargements of live stock investments. A droughty month, a day's hot wind or the hail-storm of an hour may undo the labor of an entire season and send want and poverty to the farmer who is dependent on the result of a single farm product. How different is the situation, under a like visitation, of the mixed farmer, who, in the event of failure of one crop, has another yielding good returns ; or should the year be so unfavorable as to end in a loss of the entire sea- son's work — a calamity which sometimes happens to the farmers of any land — how fortunate is the man who can fall back on his herds and flocks , and in this manner bridge over the days of agricultural disaster. Then, looking at the matter in another light, even with favorable crop seasons and an abundant yield of farm products, the farmer who combines stock growing with his other farm operations has a wonderful advantage over his neighbor who devotes his labor's solely to the tillage of the soil. He obtains a greater profit out of his farm products by feeding to stock and marketing his fat cattle. He is independent of wheat corners and the rapacity of transportation companies — he evades the many profits paid the grain buyer, the elevator and mill man and the carriers, by feeding his grain on the farm to his horses, cattle, sheep or hogs, as the case may be — for all of which, when ready for market, there is a steady demand at home. Nowhere in the world do the native grasses grow with more luxuriance and richness than in Dakota — and the crop is a never failing one. The prairie everywhere is covered with a luxuriant growth of buffalo, gramma, and blue stem grasses, equal for grazing and hay to the tame va- rieties of the East. The entire hay crop of the Territory, (which in 1885 amounted to 1,527,987 tons,) is made from the native grasses. One has only to find a vacant piece of prairie and his hay crop w T ill cost him but the expense of cutting and stacking. These native grasses cure to hay upon the ground, and stock will fatten on the prairies almost as rapidly as they do in the East feeding on grain. The grass retains its richness throughout the year — even where uncut — and in many places stock is kept through the severest winters solely by pasturing on the plains. It is mowed at any time, making quite as good hay in the fall as during the summer months. Millions of acres of this native forage grow, cure, and go to waste an- nually, uncut and unfed. If the gras?, growing on the prairies of Dakota could all be utilized and turned into beef, it would supply the markets of 132 RESOURCES OF DAKOTA. the world. The native hay crop will add millions to the annual profits to be derived from that source when the day arrives that not an acre is al- lowed to w go to waste. r There never has been a time in the history of Dakota, when the prairies did not furnish an abundant supply of fodder for stock — no matter how disastrous might be the effects of the weather on the farm crops. The dryer the season the better the quality of the native grass, is the universal verdict of the ranchmen who were wont to herd their cattle on the prairies long before Dakota was thought to be fitted for agricultural pursuits. As has been said, large herds of cattle are annually kept on the prairies without grain or other fodder — grazing on the native grasses the entire season-Miheir only shelter from the storms of winter being found in the breaks of the surrounding hills. Along the Belle Fourche, the Cheyenne and their tributaries, on all sides of the Black Hills; the Little Missouri, and the great stretch of un- settled country to the west; the Mouse river and the coteaus of the north, many thousancFkead of cattle, horses and sheep are wintered in this way. l w . The stock is simply branded and then turned out to "rustle," in the stockman's parlance, and not the least attention is given to the herd until the spring " round-up " of the following year. A " round-up " is where a collection of cow-boys, representing the various ranches of the district, meet at an agreed time and place for the purpose of driving all the stock together, when each owner separates his particular brand from, the rest, brands the calves and again turns the herd out on the prairies. The next "round-up" occurs later, when the stock is again encircled and the fat cattle cut out of the herd to be driven to market. This is the manner in which the large cattle ranches are managed, where immigration and the settlements have not compelled its abandonment. However, the rapid encroachment of the farmer on the stockman's do- main has driven the ranches to a rather limited district in comparison with the great area over which, at one time, his herds roamed at will. It cannot be long ere cattle ranching in Dakota, on the great scale of the earlv day, will be one of the lost arts. The rush of immigration spreading over every section of the Territory will render necessary the herding of the flocks on the prairies through the spring, summer and fall; the feeding of native hay in the winter season and the furnishing of other shelter from the weather than the hills and breaks, as is done in the older settled sections. In addition to the wonderful nutritive qualities of the native grasses, the dryness and equability of the climate has much to do in making the. raising of stock successful in the highest degree A writer has truthfully said: " The climate (of Dakota) can be called the chief advantage of the country for stock raising, the summers being of about the temperature of the much noted stock raising regions of the Old World, and the winters cold sunny and bright. It is the cold, combined with the absence of high RESOURCES OF DAKOTA. 133 humidity, that gives the country such advantages for stock raising, over more humid and warmer localities, for the natural habitat of all our useful domestic animals, the horse, ox and sheep, is in a region having precisely the same climate as this, the steppes and plains of Central Asia, north of latitude 47°. Probably more cattle range on these unsheltered plains to- day than in America. Atkinson, in his travels, mentions the tens of thousands of head grazing around the steppes which surround Lake Baikal in latitude 52°." Rain is almost entirely unknown between October and April; stock are seldom wet during the cold weather, and there is none of that moist air, peculiar to Eastern climates, which causes a too rapid radiation of animal heat, resulting in chilly sensations to man and beast alike. The climate being so dry and equable prevents the prevalence of those diseases that decimate the flocks and herds in so many other localities. Notwithstanding the fact that the past winter was an unusually severe one, and that many herds were on the range without shelter or provision of food, resulting in a greater percentage of loss than would have occurred had the cattle been properly cared for, the loss, during the year, was only 4 per cent.— no greater than is recorded in twenty-four of the states and territories, and less than one-half the loss as compared with some. Cat- tle on the ranges suffered heavily from the severity of the winter. Where stock are provided with the least attempt at shelter and forage, there is never any loss, and it always comes out strong and in good flesh in the spring. Were it not for the custom prevailing in some sections of the Territory of turning stock loose on the range the entire year, without pro- vision for shelter or food, we believe that the percentage of loss would be far less in Dakota than any where else in America. The need of provid- ing a rude shelter of some sort and of supplying forage, which is to be had for the cutting from the millions of acres of rich native grasses, is being impressed more strongly each year on the stock growers of the North- west. Let the stock-growers devote but an iota of the labor and expense to the care of their stock that is expended by the farmers of Iowa, Illinois, Ohio, or any state of the Union, and the raising of horses, cattle, sheep, and hogs in Dakota, becomes the safest and most profitable investment in the world. Native hay is to be had in abundance, and costs only a dollar or a dollar and a half a ton to cut and stack. We have described on another page how easily the root crops and tame grasses can be raised, and what immense yields this prolific soil returns for a very little labor. It is therefore criminal carelessness for the Da- kota farmer to neglect his stock during the winter months, as some do. It is with satisfaction we note the fact that the lesson taught by the in- clemency of last winter is being very generally heeded, and the farmers are showing a disposition to provide shelter and hay as required. Those 134 RESOURCES OF DAKOTA. TABLE SHOWING THE NUMBER OF HORSES IN DAKOTA, 1886, And their value in comparison with each state and territo y of the Union. BANK. STATES AND TER. NUMBER. VALUE. DOLLARS. 46 RHODE ISLAND g 9,955 1,061,443 ' 45 ARIZONA, 44 NEW MEXICO, 43 DELAWARE, 42 FLORIDA, 41 NEVADA, 40 CONNECTICUT, 39 IDAHO, NEW HAMPSHIRE, 37 UTAH, MASSACHUSETTS, K5 SOUTH CAROLINA, 34 VERMONT, 33 WYOMING, 32 NEW JERSEY, 31 MAINE, 30 WASHINGTON TER.. 29 GEORGIA, LOUISIANA, 27 COLORADO, ALABAMA, 25 MARYLAND, 24 MONTANA, 23 MISSISSIPPI, 22 WEST VIRGINIA, 21 NORTH CAROLINA, 20 OREGON, 19 ARKANSAS, 18 DAKOTA, 17 VIRGINIA, 16 CALIFORNIA, 15 TENNESSEE, 14 MINNESOTA, 13 NEBRASKA, ~ 12 KENTUCKY, 11 WISCONSIN, 10 MICHIGAN, PENNSYLVAI KANSAS, 7 INDIANA, NEW YORK, 5 MISSOURI, 4 OHIO, 3 IOWA, 2 TEXAS, 10,165 528,580 1 20,786 745,944 22,330 2.135.491 31,184 2,545,222 | 44,654 2.462,449 | 48,413 4,841,242 Hi 48,750 2,681,250 H 49,384 4,143,889 ■ 56,136 2,466,490 HB63.916 6,816,300 ■64,673 5,701,926 j§ggjfe,370 6,780,071 ■2,500 3,678.675 ■■ill, 648 9,463,136 ^fii 2 ' 094 8,167.650 ■B.237 6,018,458 Haft 902 8,757,335 6,534,952 HBKIIE70 7,178,918 MM 11 iMi 8,751.535 E&6 10.728,077 ■MJfefehbJOR 6,535,088 ■ggBipo 9,187,566 So' 8,910,107 10,713,012 9,045.603 10,495,908 17,618,192 M 16,725,673 18,534,948 19,667,265 29,402,052 29,349,719 26,242,445 32.983,234 38.563.565 mWtla^M3PB] ■ 55,337,053 42,263.123 49,243,727 ■ 65,017,137 44,542.180 62,389,601 71,926,052 33,642,055 , 1 ILLINOIS - ..^^1 81,152,417 RESOURCES OF DAKOTA. 135 who prefer to pasture their stock, fence with barbed wire, at a cost of about sixty cents per rod, but as a genera] thing herds are allowed to run at large on the range — or in the well settled districts a boy is employed during the summer months to look after the herd. The greatest number of stock ranches within a given area are located in the Black Hills, and numerous herds of cattle, horses, and sheep graze along the numerous streams where the valleys grow the richest of grasses, and the mountain brooks provide an abundant supply of pure, cold water. The broken nature of the country offers on all hands the best of natural shelter for stock. That the Hills would prove a paradise for stock-growers was predicted hy the Government officer in charge of the exploring expedition sent out in 1875, under authority of the Secretary of the Interior. We quote from his valuable report: "The grazing in the Black Hills is most excellent. Nine-tenths of the whole area is covered by a thick growth of the finest wild grasses. It con- stitutes the great future wealth of this region, and its value can hardly be over-estimated. * * ' California Joe,' (one of the guides attached to the expedition,) said of the valley of Spring creek: 'There's gold from the grass roots down, but there's more gold from the grass roots up.' And no matter how rich the gold placers in the Black Hills may prove to be, the great business in this region in the future, will be stock-raising and dairy farming. "Even in the clefts of the rocks, the sides of the steep ridges, and in the bottoms of the deep canons, grass is found growing, depending on the scanty soil for its sustenance, and the little sunlight that pierces through the dense branches of the trees and penetrates for a short time the depths of the gorge. ****** "I had previously been engaged in explorations in western Texas and New Mexico, but I was surprised at the quality of the grazing we found in the Black Hills, which resembled the grass growing in the oak openings in central Texas, except that it was finer and freer from weeds and the coarser and less nutritious grasses. * * * "For the requirements of the population that the Black Hills will sup- port in the next twenty years, enough hay can be procured from the wild grasses. * * * * " The wind may blow a gale over the mountain tops and exposed ridges, but in the valleys the air will be comparatively at rest, the timber cover- ing the hillsides and ridges, materially contributing toward making the valleys warm and sheltered. This will be of great advantage to the stock which may be wintered in the Hills, shelter being found every where from sudden or severe storms. * "From the secluded and sheltered character of the valleys, the abund- ance of water, and the fine quality of the grazing, the Black Hills are well adapted for dairy farming, the establishment of cheese and butter factor- ies, and the raising and breeding of fine breeds of cattle and sheep." 136 RESOURCES OF DAKOTA. To realize the complete fulfillment of Prof. Jexmey's prophecy one has only to visit the Hills and look upon the many herds of sleek cattle, fine horses and sheep to be seen in every valley and crowning every hill top. The coteaus of the Missouri— a range of low hills stretching entirely across the Territory from the northwest to the southeast — are filled with brooks ani ponds of water and furnish a paradise of native forage and splendid protection for the stock-grower and dairyman. The same is true of the country along the line of the Northern Pacific railroad west of the Missouri river, and of the Mouse river region, and the Turtle Mountains, and Devils Lake country of the north; 20,000,000 acres of vacant land are contained within the boundaries above described — almost every section of which would make as fine a stock ranch or as prolific a farm as exists any- where. Even the Bad Lands — the name by which a small stretch of country from three to twenty-five miles wide, situated principally along the Chey- enne, Grand and Little Missouri rivers, is known, has proved to be the finest stock range in the West. The surface of this region has been shaped, through various causes, such as subterranean fires, the winds and storms of ages, into the most fanta&tic and weird-looking hills, mounds, columns and valleys, and has been described as " resembling the bottom of hell with the fires put out." Mr. E. V. Smalley vividly describes the marvelous scenery of the Bad Lands in these words : "The change in the scene is so startling, and the appearance of the landscape so wholly novel and so singularly grotesque, that you rub your eyes to make sure ha 1 you are not dreaming of some ancient geologic epoch, when the rude, unfinished earth was the sport of Titanic forces, or fancy- ing yourself transported to another planet. Enormous masses of con- glomerate — red, gray, black, brown, and blue, in towers, pyramids, peaks, ridges, domes, castellated heights — occupy the face of the country. In the spaces between are grassy, lawn-like expanses, dotted with the petri- fied stumps of huge trees. The finest effect of color is produced by the dark red rock — not rock in fact, but actual terra-cotta, baked by the heat of underlying layers of lignite. At some points the coal is still on fire, and the process of transforming mountains of blue clay into mountains of pot- tery may be observed from day to day. It has been going on for count- less ages, no doubt. To bake one of these colossal masses may have re- quired 10,000 years of smoldering heat. I despair of giving any adequate idea of the fantastic forms of the buttes or of the wonderful effects of color they offer. The pen and brush of a skillful artist would alone be compe- tent for the task. The photographer, be he never so deft with his camera and chemicals, only be-littles these marvelous views. He catches only bare outlines, without color, and color is the chief thing in the picture. He cannot get the true effect of distance, and his negatives show only staring blacks and whites in place of the infinite variations of light and RESOURCES OF DAKOTA. 137 shadow effects in valleys and gorges and hollows, and upon crags and pin- nacles. Look, if you can, by the feeble aid of written words, upon a sin- gle butte, and see how impossible it is to photograph it satisfactorily. It rises from a carpet of green grass. Its base has a bluish hue, and appears to be clay solidified by enormous pressure. It is girdled by 1 ands of light gray stone, and black Tgnite coal. Its upper portion is of the rich, red color of old Egyptian pottery. Crumbled fragments strew its sides. Its summit, rising 300 feet above the plain, has teen carved by the ele- ments into turrets, battlements, sharp spires, grotesque gargoyles, and huge projecting buttresse s — an amazing jumble of weird architectural ef- fects, that startle the eye with sue gesl ions of intelligent design. Above, the sky is wonderfully clear and blue, the rays of the setting sun spread a rosy tint over the crest, and just above its highest tower floats a little flame-colored cloud like a banner. When I say there are thousands of these buttes, the reader will perceive that the Bad Lands of the Little Missouri are a region of extraordinary interest to the tourist and artist." The country is full of such plateaus, and in the valleys is found the best of protection for stock. Mr. A. T. Packard, editor of the Bad f ands Cow Boy. writes as follows of this region: "There is a very general opinion in different parts of the country, that the Bad Lands are the most sterile and uninhabitable region on the face of the earth. The writer well remembers the impression of them he obtained in his very youthful days from the study of Guyot's geography. To the stock-raiser and coal miner, however, this is the king country of the world. In no other place are there to be found so many favorable conditions for the raising of stock. Bunch and buffalo grass cover almost every inch of the ground. 1 he raw sides of buttes are the only places where splendid.grazing cannot be found. On many of the buttes, however, the grass grows clear to the summit, the slopes being the favor- ite pasture lands of the cattle. Generally no hay need be cut, as the grass cures standing, and keeps the cattle in as <:ood condition all winter as if they were stall fed. The only reason for putting up hay is to avoid a scarcity of feed in case of heavy snow. This very seldom happens, how- ever, as very little snow falls in the Bad Lands. In spite of the numer- ous cuts of the railroad there never has been a blockade in the Bad Lands, although they are common over all the rest of the road. A curi- ous fact with cattle is that the ones that have been here a year or two, and know how to rustle, will turn away from a stack of hay, paw away the snow from the grass, and feed on that exclusively. Even in the dead of winter a meadow has a very perceptible tinge of green." The rapid increase of fine stock in the Territory and the tendency to improve the grades by importing high-bred animals is very noticeable of late years. In those sections of Dakota Fettled for any length of time the numerous herds of Herefords, Polled Angus, Shorthorns, Holsteins or Jer- sey cattle, Percheron, Cl\ desdale or English shire draft horses, speed 138 RESOURCES OF DAKOTA. animals of excellent pedigree, and well-bred mules, sheep and swine, bear testimony to the fact that the Dakota farmer appreciates the value of breeding high classed stock. At the Territorial fairs (one held in north Dakota and one in the south) and the different fairs of the various coun- ties, the display of fine stock called forth the wonder and admiration of the Eastern visitor, who w T as forced to admit that as respects her graded stock Dakota is not excelled by many of the old states. The indications are that in a few years the -Territory will have built up a world-wide rep- utation for the good quality of its horses. The farmers are realizing that it costs but little more to raise a high-class oraft animal than an ordinary scrub, and everywhere one hears of the importation of the best grades of brood mares and finest pure bred stallions. Farm work requires heavy draft horses and the intelligent farmer understands the value of crossing with the large and powerful French, English, or Scotch breeds. It will not be long until Dakota will ship to the East a breed of horses unequaled in energy, form and endurance. AVith so favorable surroundings for the profitable carrying on of the enterprise it is somewhat difficult to explain satisfactorily why our people have delayed until very recently the business of sheep-growing. Those who have engaged in this branch of the stock business are re- markably well satisfied with the venture. It is asserted that in no other country have better results followed the growing of sheep than in Da- kota. The absence of swamps, and damp, rainy seasons, give- security from the foot-rot, scab and other diseases so fatal to sheep. The following extract, from ■> publication, well known, an authority on stock matters, will be of interest to all who contemplate the handling of sheep: " Ten years ago there were literally no flocks of sheep in Dakota. It is true that the great bulk of southern Dakota was not then settled; but there was a tier of counties along the Missouri river on the south, and Big Sioux valley on the eastern border that was settled; and, although the uniform weather and dry winter atmosphere were known to be favorable to sheeD-raising and wool-growing, little or no effort was made to intro- duce sheep. About ten years ago the German-Russians began settling in southern Dakota and they at once introduced sheep husbandry and made it a success. The kinds now kept are largely Merino, but occasionally a flock of South Downs or Leicesters is found. The flocks are generally healthy and the fleeces fairly heavy. Wool finds a ready market in any of the larger towns in the Territory, and is mostly shipped East. Nu- merous woolen manufactories are springing up in Dakota, but the produc- tion is greatly in advance of the home market. Fortunately, wool is one of the products of the farm that will bear shipping for a considerable dis- tance. Mutton is in good demand and brings a fair price. It is possible the larger framed sheep of Canada would be more profitable. They are hardy, and, when full grown and fattened, a carcass frequently weighs from RESOURCES OF DAKOTA. 139 100 to 125 pounds. The climate of this section makes the flocks exceed- ingly prolific. It is an easy thing to accumulate a large flock of sheep in a few years. '* Sheep are herded in summer in the same manner as horned cattle, and not unfrequently by the same person — especially if the flock of sheep be small and the herd of cattle i,^ not large. In winter the flocks are pro- vided with corrals and sheds for protection from storms, and are fed with the wild hay of the prairie, upon which they subsist without grain. It is no doubt true that with better c ire of the flocks the profit of sheep hus- bandry would not only be surer, but greater. But the first settlers in any country are seldom prepared to obtain the best results from their labors, for want of time and means to Droperly provide for their flocks and herds. Notwithstanding all the lack of facilities for caring for stock by the pio- neers of southern Dakota, sheep-raising has proved a profitable industry, and one that in the near future will be largely increased " Mr. A. S. Hall, a farmer of Hand county, encourages his neighbors to a deeper interest in sheep-raising, and says: " I have never lost a single sheep from disease and rarely more than two per cent, from any cause during a year. My greatest loss has always been of old ewes, as I was always looking more to the increase of my flock thai; per centum of loss. Began the winter of 1886-7 with 3i5 of all ages, at least fifteen of the number belonging to the class of ' relics.' I fed during the winter the headed straw from about 100 acres of wheat, twenty-five acres of millet hav, and twenty tons of weedy, wild hay, that was not fit for other stock. No grain whatever. The account is about as follows: RECEIPTS. Wool, 2,547 pounds at 20 cents 1510 40 Lambs, 140 at $2 280 00 Pelts, 5 at $1 5 00 Total : $795 40 EXPENDITURES. Millet hay, $4 per acre 100 00 Straw and wild hay 75 00 Labor .-.' 25 00 Interest on investment, including shed 100 00 Total $300 00 Balance 495 40 A report is received from the owner of a herd of 1,800 sheep who brought his flock through the past winter— the severest known for years — without the loss of a single one. In the Black Hills many ranches are devoted exclusively to sheep rais- ing, and with the most satisfactory results. 140 EESOURCES OF DAKOTA. TABLE SHOWING THE NUMBER OF MULES IN DAKOTA, 1886, And their value, in comparison with each statu and territory of the Union. RANK. STATES ANI) TEH. NUMBER. VALUE. DOLLARS. 40 WAS HINGTON TEH.. | 1,231 102.247 39 NEVADA, 1,657 121,251 38 ARIZONA, 37 IDAHO, 36 WYOMING, 35 OREGON, 34 UTAH, 33 DELAWARE, 32 NEW YORK, 31 MICHIGAN. 311 WEST VIRGINIA, 29 WISCONSIN. 28 COLORADO. MONTANA, 2G NEW JERSEY. 25 MINNESOTA, 24 NEW MEXICO. 23 FLORIDA, 22 DAK0TA,=S3Di 21 MARYLAND, 20 PENNSYLVANIA, 19 OHIO. 18 VIRGINIA. 17 CALIFORNIA. 16 NEBRASKA. 15 IOWA, 14 INDIANA, 13 SOUTH CAROLINA, 12 LOUISIANA. 11 KANSAS, 10 NORTH CAROLINA, 9 ARKANSAS, KENTUCKY. 7 ILLINOIS. 6 ALABAMA, 5 GEORGIA, 4 MISSISSIPPI, 3 TEXAS, 1,863 ] 37,862 2,436 210,714 2,850 198 887 3,155 229.086 Hi 3,579 215,082 4,061 480,130 HBt 5 ' 158 571 ,860 ■I 5,486 556,208 BH 6,540 495.399 8,010 754,877 1 8,165 685,224 \ 9,229 662,181 HUH 3,407 1,136,749 HSBSl 0,447 1,036,624 ^^L0 912 520,501 MUIUIl.789 1,107,284 H^ffil-964 (,(94,622 HHK&358 1,284,544 HBBH>(370 2,615,691 HHE£3479 2,153,571 nkiM^™ 3,058.096 nmm^ 84 3.035.912 mmamssB^s 3,716,460 SEfe 4,186,822 4,495,201 StM/SBm 6.888.383 6,876.876 MlJiaiMLUiaffSalB 7.320,901 Pfflffiffl^lffftffiBl 6.994.096 ?,■ i^Y ., ■;, :-r=S , , '_';'-; ' ; ■-.■', 8,566.439 8.883,535 10,476,670 11,194.624 13.980,552 12.953.958 9,037,232 HH 13,521,572 2 TEN NESS 1 MIsSSSliD ^9,633 RESOURCES OF DAKOTA. 141 From the indications of the present season, Dakota will soon be enti- tled to as prominent a rank in the list of states and territories with regard to mutton and the wool clip as she now takes when other farm products are considered. Probably there is no one line of farming ventures in the Territory' which has received the sudden enlargement of patrons and investments : as that of the sheep business. Especially is this true of the counties of the Black Hills, those bordering the Missouri river and sections of north Dakota, Many herds were shipped into the Territory during the past summer, and it is evident that there has been a widespread education of the farm- ers to the advantages of raising sheep in connection with the usual farm operations of the prairie. For 1886 — a very disastrous season to stock men — the losses of sheep in Dakota were but 6 per cent., while in some of the states they were as high as 11, 12 and 13 per cent. The rapid expansion, during the year or two past of the area planted to corn has naturally carried with it a marked growth in the number of hogs on the farms of Dakota. From January 1st, 1886, to January 1st, 1887, this increase amounted to 20 per cent. — the undoubted result of the en- largement of the corn fields of the Territory. In 1880 there were but 63,394 hogs in Dakota— a number which had in- creased to 427,176 in 18S6— or nearly 700 per cent. Hogs do well on the native grasses during the summer and the fall, and throughout the year are remarkably free from the complaints' usually af- fecting swine. Hog cholera is a disease unknown in the Territory. The losses for swine for the year ending January 1st, 1887, were 6 per cent. — being less than occurred in twenty-five of the states, where the losses ran all the way from 6.5 to 27 per cent. For many years the growers of stock will find a good demand at home for the surplus of their herds. The building of railways and the rush of immigration furnish a constant demand for mules and draft horses. Every day witnesses the importa- tion of many car loads of work horses into Dakota from neighboring states — horses, the sale and profit of which should be realized by our own farmers. Dairies and creameries are springing up in every locality, and have in- creased the value of milch cows in their vicinity, at least twenty-five per cent. There is a strong demand for heifers for breeding purposes, oxen for farm work and fat steers for beef. Pork-packing establishments are increasing in number, and find a ready market at home for every article manufactured. The mining districts of the Black Hills and the military posts and In- dian agencies require immense quantities of beef and hog products, the greater portion of which is now brought in from abroad. 142 RESOURCES OF DAKOTA. Following are the views of some of the noted stock-growers of the North- west on the question of mixed farming, the advantage of the climate, the richness of our native grasses, the relative profits of raising cattle and horses, etc., etc. Dr. C. J. Alloway, Territorial veterinary surgeon, who has some fine herds on his farm, near Grand Forks, says: " Phenomenal as has been the growth of wheat culture in Dakota, it is admitted on all sides that the cattle industry bids fair to more than equal it in the rapidity with which it is taking hold. The experiments of a few practical men in the past three or four years have so fully demonstrated the adaptability of the country to this industry, that those acquainted with these facts did not hesitate to make the breeding of live stock either an important part of their agricultural undertaking, or, as hundreds have done, an absolute specialty of it. '■' It has been pointed out that these vast grazing areas of the Northwest were the natural feeding grounds of the American buffalo, and it is reason- able to presume that this was the case from the fact of their being so ad- mirably adapted to that end. Had ihis soil not been fertile, abundantly productive, and its grasses nutritive, this page in Dakota's history would certainly have been wanting. A combination of circumstances have con- tributed largely toward the opening up and advancement of the live stock interests of Dakota and Minnesota Chief among which are the quantity and quality of the wild grasses to be met with everywhere, the purity and abundance of the water, the ease with which root crops of all kinds can be grown, the favorable conditions of the climate, and a steady and increasing demand for beef, butter, cheese and milk. Another, and an important consideration had not a little to do with this comparatively new venture in agriculture in Dakota, namely: The fact that the great major- ity was depending solely upon the production of one article. It matters not whether that product brought a high price or a low one, the denizen of Dakota always had to pay top prices for all the necessaries of life, not excepting flour. Pork, beef and provisions of every kind had to be ship- ped in, and, as in the case in all newly-opened regions where communi- cation is imperfect and more or less difficult, provisions were necessarily hard to procure, and correspondingly high in price. Chicago furnished us with beef, pork, canned meats, at prices that were always high and that varied little, while the same commercial center bought our grain at figures that harmonized w T ith the caprices of the most powerful wheat ring on earth. To put this in another light, the farmer of Dakota invaria- bly disposed of his wheat at the lowest market price, whereas he pur- chased meats and other commodities, that he could as readily grow as wheat, at the highest figure. " The agriculturist of the Northwest has seen the error of his ways, and as a consequence is branching more or less extensively into mixed farm- ing, and a great many that have the capital are going solely into the RESOURCES OF DAKOTA. 143 growing of live stock. Evidence of this radical change is apparent in every county in north Dakota, and, no doubt, is the same in the central and southern portion. * * "Prominent among the auxiliary enterprises developed by the growth of the live stock industry of the Northwest, is the establishment of the St. Paul Union stock yards, at South St. Paul, and the organization of a stock company of a similar nature at Minneapolis; the former with a capi- tal of one and a half millions and the latter of one million dollars. "The plant in the St. Paul Union stock yards is of the finest and most improved, and their entire equipment is unsurpassed in any country. This company has not only mammoth slaughtering, packing and render- ing houses, but has large buildings for feeding and bringing to perfection animals that are not yet ready for market. Elevators, feed-carriers > hand- some offices, a bank and hotel, also form part of this important adjunct to the live stock intere sts of Dakota. "The Minneapolis yards will also be on a very large and costly scale. Ground has already been broken and the various buildings are in course of erection. These stock yards are intended to be second to none in point, of accommodation and convenience, and will be ready for operation in the spring of 1888. To the cattle, sheep, and hog growers of the great Northwest these extensive establishments are of paramount importance, and are a substantial evidence of the views held by the capitalists of these two great Weatern cities of what they expect of the live stock traffic of this favored land of ours. " Heretofore the grower of beef, pork, or mutton was compelled to ship his produce to Chicago or Kansas City, whereas in the future he can al- ways find a ready market at one or the' other of the twin cities. And he will further have the benefits of competing markets in close proximity to each other. " While Minneapolis is to-day the greatest flour emporium in the world, in less than ten short years her packing business is certain to equal, if it does not surpass, that of her wheat and flour. The coming decade will bring more marvelous changes to the farmer of Dakota in the matter of live stock than did the heretofore unparalleled increase in the production of wheat." The preparation under way on so vast a scale, by the cities of St. Paul and Minneapolis, with the purpose of controlling apart of Dakota's heavy and increasing traffic in live stock, is being repeated with even more energy and investment, if possible, by a very near neighbor, also a suc- cessful bidder for a share in the division of the live stock interests here- tofore so largely in the hands of Chicago, viz. : Sioux City, Iowa. The Union stock yards of Sioux City, although of recent establishment, trans- act a daily business, during the shipping season, exceeding $30,00.0. Every facility science and experience has invented for the proper and easy handling of stock, is here provided, including banks, hotels, offices, 144 RESOURCES OF DAKOTA TABLE SHOWING THE NUMBER OF HOGS IN DAKOTA, 1886, And their value, in comparison with each state and territory of the Union. RANK. STATES AND TEK. NUMBER. VALUE. DOLLARS. 47 WYOMING, 2,750 17.596- 46 ARIZONA, 1 13,700 54,804 45 RHODE ISLAND 14,107 130,130 44 NEVADA, 14,543 77,r?9 43 MONTANA, 20,263 119,163 42 NEW MEXICO, 20 990 131,505 41 COLORADO, 21,290 146,424 40 IDAHO, 28.100 147,525 39 UTAH, 28.656 237,052 38 DELAWARE. m 42,654 304,977 37 NEW HAMPSHIRE, 53,860 504, ?38 36 CONNECTICUT, 61,164 538,245 35 MAINE, 71,056 611,080 34 VERMONT, | 74,856 589,688 33 MASSACHUSETTS. filial 76,840 775,319 32 WASHINGTON TER.. jPffjjl 90,152 384,094 31 NEW JERSEY. 1.574,526 30 OREGON, iPPSs 5 ' 879 656.523 29 MARYLAND, 1.789,077 28 FLORIDA, m 8,108 729,768 27 MINNESOTA, g|,918 1,943,730 26 DAKOTA, » 176 2,314,013 25 WEST VIRGINIA, 'JI&778 1,780,448 24 SOUTH CAROLINA. |g- fa. 66 2,068,625 23 LOUISIANA. 1,754,567 22 NEW YORK, JgB8 ®8 5,145,331 21 VIRGINIA, 3,237,570 20 MICHIGAN, 4,794,419 19 INDIAN TER., 2,210,000 18 WISCONSIN. 5 314.284 17 CALIFORNIA, 3,841.409 16 PENNSYLVANIA. - > 7,750,178 15 MISSISSIPPI, 3,345,516 14 NORTH CAROLLNAjB 4,286,700 13 ALABAMA, 3 882 703 12 GEORGIA, 4.405,098 11 ARKANSAS, 4,030 203 10 KENTUCKY, ■'...,,-'■.'.■'•'•'." ■J ■^^.■■'■■■■^■:r-':f 6,905,247 9 TENNESSEE, | 5,022,181 8 KANSAS, • 11.055.240 7 OHIO, 12,067,882 6 nebraskJSH 13.073,336 5 INDIANAgf 13,396,880 4 TEXAS, H SS^^i^^E 7,090,476 3 LLLiijBi^a^BMpB 8^19,997,572 2 BBSpi mb^bm ■QKE32Q7 BtBISlSKlHB^MMHiiBiillUlBB RESOURCES OF DAKOTA. . 145 ample yards, arrangements for feeding, housing, loading and unloading, etc. The six beef and pork-packing establishments of Sioux City, repre- sent an outlay, covering the several plants, of more than a million dollars, with a capacity to prepare for market, daily, 1,500 head of beef cattle and 15,000 hogs, and transact a yearly business amounting to the enormous sum of $23,000,000. These heavy investments made by the cities of St. Paul and Minne- apolis to handle the live stock shipped from the northern counties, and by Sioux City as a market for the beef and hogs of south Dakota, is of itself the weightiest proof of the rapid increase in the number of farm animals in the Territory. Extract from a speech delivered at St. Paul by President J. J. Hill, of the St. Paul, Minneapolis and Manitoba railway, himself a breeder of fine stock ■ *.#*'**'***■* "A few years ago it was said a man was pretty far from home when he was where he could not raise corn. Now a man goes a good way from home and finds he can raise corn. It is hard to say what you can and what you can not raise. There is one thing the people lose sight of when they undertake to feed cattle — thM2 1,968,838 MBbVablSfe 5,213,558 5.485.187 3,670.173 5,958,098 [ 11,533,675 7,718,928 1,192 148 RESOURCES OF DAKOTA. gregate gain in the 153 days, of sixty-three head, to be 20,055 pounds, an average of two and one-twelfth pounds per day, or 318f pounds per head. Analyzing the record I ascertained that the yearling steers, (fourteen head,) had gained 60 4-5 per cent, on their spring weights; four head of two-year-olds, 47 per cent.; and five three-year-olds, 31 percent.; twenty- one yearling heifers, 85 per cent.; nine two-year-olds, 52| per cent.; and ten barren cows, 27 2-5 per cent. The general average gain of the lot was 47 4-5 per cent. Thus I obtained an answer to my first question. " Eight head of milch cows were put in a small fenced field of some thirty acres, that during the entire grazing season afforded more than the needed supply of grass, from which I was satisfied that three acres per head was sufficient for summer pasture. The second question was answered. "In passing, let me say that our pastures are entirely of native grass, good until October 1st, when failing somewhat, the stock is brought into the yards at night, given some corn fodder and allowed free access to ricks of freshly threshed oat straw; but with the exception of our pure-breds we have never put our stock of cattle in barn for either shelter or feed until the 1st of November. * * * * * * "The question, which pays the best, horses or cattle, naturally comes to the front. My records give me some figures upon which to work, and from them I make up the following: " Firs'. Five head of 1883 steer calves from native heifers by a pure- bred short-horn bull, show an aggregate weight, May 17, ,1884, of 2,320 pounds; November 1, 1885, 5,515 pounds. " On pasture during the summers of 1884 and 1885, for which I allow three acreseach, each year, I charge, use of thirty acres at $5 per acre, 8 percent., $12. In the barns, from November 1, 1883, to April 30, 1884, and Novem- ber 1, 1884, to April 30, 1885, cost of winter feed, labor, and interest on cost of building $10.50 each, each winter, in all, $106. Total cost of the five head $118.00 Their value Nov. 1, 1885, 5,515 lbs. at 3§ 192.97 Showing profit of (63 per cent.) $ 74.97 "Second. Among my purchases in May, 1880, was a large, fine, seven- eighths bred short-horn cow, then in calf by a pare bred bull, for which I paid $100. For convenience, I named her Fatty. May 1, 1885, we have: Fatty, then in calf, valued at $ 75 Fatty 2d, on 1880 calf, in calf May 1, 1885 75 Fatty 3d, on 1881 calf, in calf May 1, 1885 :. 75 Fatty 4th, on 1882 calf, in calf May 1, 1885 65 Fatty 5th, on 1883 calf, heifer 50 Fatty 6th, on 1884 calf, heifer 35 Fatty, steer, on 1883 calf, from Fatty 2d 35 Fatty, steer, on 1884 calf, from Fatty 3d 25 In all, eight animals valued at $435 RESOURCES OF DAKOTA. 149 " My estimated cost of keep on the lot to May 1, 1885, was $240; shrink- age in value on the old cow, $25; profit $170. Sixty-four ner cent, in aver- age of two and one-half years, about 26 per cent, per year. " Third. In June, 1880, I purchased two good, common mares, .one in foal, that cost, Jaid down at the farm, $340. On the first of December, 1885, I find the two mares in foal by our pure bred French draft stallion, Valued at $ 300 One colt in 1881, sold in 1884 for 200 Two colts in 1882, sold in 1885 for 300 Two colts in 1883, sold in 1885 for 335 Two colts in 1884, on hand, valued at 225 Two colts in 1885, on hand, valued at 100 The total valuation amounting to $1,460 " During the five and one-half years these mares were steadily at work, both summer and winter, more than earning their keep, but charging up their keep as if kept only as brood mares, the debits would be about as follows: Keep of mares and colts, including labor and interest on cost of buildings $420 Shrinkage on the old mares 40 Total cost $460 " A clear profit of $1,000, 217 per cent, on an average of not to exceed three years." The total number of farm animals in the United States as compared with the figures of last year, are as follows: Stock. 1886. 188; Increase or decrease. Horses 12,077,657 12,496,744 Mules 2,052,593 2,117,141 Milch cows 14,235,388 14,522,083 Oxen and other cattle 31,275,242 33,511,750 Sheep 48,322,331 44,759,314 Swine 46,092,043 44,612,836 + + 419,087 64,548 286,695 2,236,508 3,563,017 1,479,207 The average values of ten years past are given in the table below. Years Other Horses Mules Cows .ot+ip Sheep Swine 1878. 1879. 1880. 1881. 1882. 1883. 1884. 1885. 1886. 1887. | 58 16 52 41 54 75 58 44 58 52 70 59 74 64 73 70 71 27 72 15 63 56 61 69 71 79 84 82 71) 78 70 $ 06 26 79 35 49 22 38 60 91 26 41 | 17 14 $ 2 25 21 73 15 39 2 07 23 27 16 10 2 21 23 1)5 17 33 2 39 25 89 19 89 2 37 30 21 21 SO 2 53 31 37 23 52 2 37 29 70 23 25 2 14 27 40 21 17 1 91 26 08 19 79 2 01 4 98 3 18 4 28 4 70 5 98 6 75 5 57 5 02 4 25 4 48 150 RESOURCES OF DAKOTA. DAIRY PRODUCTS. The excellent quality of native forage results in the production of as sweet milk and butter as can be found in the world. The yield of milk is in excess of what one would expect from prairie fed cows and the quantity and quality are kept up through the season with a constancy quite sur- prising. This follows, undoubtedly, from the rich and nutritious proper- ties of the buffalo and gramma grasses, and from the fact that the prairie forage cures upon the ground, retaining its strengthening qualities the year round. X. A. Willard, of Little Falls, New York, a standard authority on dairy- ing, in his work, " Practical Dairy Husbandry," says: "The great American dairy belt lies between the fortieth and forty- fifth parallels of latitude. -x- -X- *'*•''** " The characteristics of a good dairy country are high, undulating sur- faces; numerous springs and streams of never-failing water; a soil reten- tive of moisture; a sweet and nutritious herbage that springs up spontan- eously and continues to grow with great tenacity; a rather low average temperature; frequent showers rather than periodical droughts; and suf- ficent covering of the ground in winter, to protect grass roots so that the herbage may be permanent or enduring. * * * " In my opinion, upon this Northern belt of dairy lands, there is no de- scription of farming promises better prospect of remuneration than the dairy." It costs but little to keep milch cows in Dakota. The ranges are bound- less in summer and hay or root crops for winter feeding cost but a trifle. Farmers are turning their attention more and more to the enlargement of their herds and as a result are deriving no small part of their income from the sale of milk and its products. In 1880 Dakota produced 2,000,955 pounds of butter, 39,437 pounds of cheese and 415,119 gallons of milk. Five years afterwards these amounts had increased to 10,804,260 pounds of butter, 116,557 pounds of cheese and 1,860,358 gallons of milk, while the number of milch cows on the farm, had increased almost 500 per cent. The growing interest among the farmers in stock raising and their ap- preciation of the profits to be derived from a herd of cows has led to the establishment of a great number of creameries and cheese factories in different sections of the Territory. These factories send out cream w T agons and gather the cream from a wide area of country — paying the farmer for it a price equivalent to about a shilling a pound for butter. A creamery will use, as a general thing, the milk from a thousand or more cows, scattered among the hundreds of farmers of the vicinity. Dakota, with advantages similar to her neighbor on the east, Minnesota, where the farmers of the southern and central portion have been lifted from poverty to prosperity by that great mortgage lifter, the cow, is des- tined to become one of the greatest dairy states of the Union. When RESOURCES OF DAKOTA. 151 our farmers, without exceptions, keep cows, sell butter, cream and cheese and raise stock in connection with their farming operations — then indeed is the prosperity of the Territory assured. Comfortable homes, large barns and the ability to meet every obligation are the rewards to the farmers who take a part of the investment from the wheat fields and expend it in cattle, horses, cows, sheep or hogs. Hon. Norman J. Coleman, the present United States Commissioner of Agriculture, is with us in our endeavors to impress on the minds of the new comer that in mixed farming lies the surest road to success. These are his words in a recent address to farmers: " Go to the great state of New York, the New England states, to Iowa, Minnesota, and other states, and as you travel through the country you can tell when you come to the dairy region. There you see the finest residences, the most comfortable and best equipped stables and buildings, the best fences, the best surroundings, and if you can get into the bank you will find the largest bank accounts credited to the dairymen. Their farms, in the East, are worth from one hundred to two hundred dollars per acre, notwithstanding the long winters, when they are compelled, on account of the severity of the weather, with the thermometer sometimes down to thirty or forty degrees below zero, to feed so many months of the year." WOOL CROP. lbs. 1870 _ _j 8 ,810 157,025 152 RESOURCES OF DAKOTA. MINERAL RESOURCES. We have at present but a faint idea of the real extent and importance of Dakota's mineral wealth, owing to the lack of Government surveys and the comparatively short time the Territory has been settled. The average Dakotaian has been engaged in the work of earning a home, and in efforts to bring the surroundings up to a standard of civilization para- mount to that of the locality whence he came; he has had but little time or inclination to study out what might be" : hid away beneath the earth's surface. However, enough has already been discovered, (and these discoveries have been more in the way of an accident than the re- sult of any systematic or learned investigation,) upon which to found a reasonable prediction that nature has distributed the valuable and useful minerals throughout the length and breadth of this vast Territory with the same bountiful hand that has provided 'the richest of soils and the most healthful climate in all the world. Deposits of coal, petroleum, salt, tin, iron, copper, lead, marble, granite, mica, asbestos, potter's clay, besides the precious metals — in fact, almost all of earth's treasures— so far discovered and utilized by science, are known to exist within the boundaries of Dakota. But, up to this time, only the precious metals, gold and silver, have been successful in wean- ing the inhabitants from such pursuits as go hand in hand with the devel- opment of a purely agricultural community. The recent discoveries of wells of natural gas and the completion of the many lines of railroad projected in every direction, which will bring with- in reasonable contiguity the immense coal fields and valuable mineral de- posits of western Dakota and the markets of the eastern part, must certainly result in the rapid development of manufacturing interests in the Territory. Capital is far-seeing, shrewd and aggressive, and such opportunities as Dakota offers to-day for lucrative investment in the development of the mines of mineral wealth now lying dormant everywhere, will not go begging long. The day is not far distant when the amount of capital invested in mining and manufacturing industries will bear no mean relationship to the agri- cultural and stock interests of the Territorv. RESOUECES OF DAKOTA. 153 NATURAL GAS. The term " natural gas," Prof. Weeks says, in his report to the director of the United States geological survey, "is the one almost universally ap- plied to that mixture of several gases found by drilling in certain sec- tions of the country; chiefly, and in the largest quantities, in western Pennsylvania and northern Ohio." The gas is mainly marsh gas, ethane, hydrogen, and nitrogen, and the term natural gas was applied to distinguish it from the artificially pre- pared gases of commerce. Natural gas is found in varying quantities all through the United States, from the Hudson river in the East, to Cali- fornia in the West. Its earliest economic use in this country was, probably, in lighting the village of Fredonia, Chautauqua county, New York, in 1821. For many years gas had been observed issuing from the crevices of the slate rocks along th ebanks of the creek on which Fredonia is built. A well, one and one-half inches in diameter, was put down twenty-seven feet, and the gas conveyed to the buildings in which it was used, in wooden pipes. In 1824, on the occasion of Lafayette's visit, the village was lighted with natural gas. The first use of natural gas in manufacturing, was in boiling salt, some twenty years after this, in tbe Kanawha valley of West Virginia. It was not until 1883 that natural gas began to be used extensively as a fuel at Pittsburg and elsewhere in Pennsylvania and Ohio. Now, few of the important manufactories of the cities of Pennsylvania and Ohio, so situated as to obtain a supply of gas cheaply, use any other fuel. The amount of coal displaced by the use of natural gas in 188), is represented by a money value of $5,000,000. That natural gas is stored beneath Dako- ta's surface, there is no longer any doubt, it has already been found in several places in sufficient quantities to use for heat and light, with proper development. So far, the discoveries were the result of accident, while sinking wells in search of water, and no attempt has been made to save or utilize the gas. If we except the well at Fargo, Cass county, which was sunk down several hundred feet last fall, when cold weather caused a suspension of operations — there has never been any effort put forth to determine the extent and quantity of natural gas underlying the Terri- tory. Preliminary steps have been taken to immediately develop and utilize the flow at all three of the localities where the actual existence of natural gas is being demonstrated daily, by its escape from rocky fissures or from excavations made in search of water, viz.: Fargo, in Cass county, Jamestown, in Stutsman county, and in the southern part of Sully county. Stock companies of ample capital, have been formed in the three places named, for the purpose of importing from the oil and gas fields of Penn- sylvania — the necessary tools, and experienced help to thoroughly test the value and extent of the supply. Capitalists familiar with the oil and natural gas districts of the East have carefully examined the geological for- 154 RESOURCES OF DAKOTA. niation of these Dakota localities, and nave prospected the existing indi- cations with a unanimous verdict to the effect that the same conditions are found here, as have been observed to be essential to the gas fields of Pennsylvania and Ohio. The first record we have of the discovery of natural gas in the Territory, was that made by Mr. Oberlin, a farmer living in Sully county, about five miles northwest of the city of Blunt, who had dug a well some seventy- five feet deep, and not striking water, continued his investigation 135 feet deeper, with a two-inch auger. At this depth (something near 200 feet), the auger penetrated a vein of what the farmer termed "foul air," from the fact that the poisonous effects of the strong flow came very near caus- ing his death. The hole was filled up and efforts begun to find water in another spot, with the same result as before, of a flow of " foul air," and the filling up and abandonment of the well. What the farmer pronounced " foul air " was natural gas, as has been demonstrated by later discoveries in the same vicinity. The next instance of a find of natural gas occurred during the summer of 1885, and not far from the one first recorded. AVe give the following published account of the discovery : " There was no mistaking the real nature of the substance in this in- stance. The escaping gas made a noise resembling that of an engine blow- ing off steam, and could be heard as far. This flow threw out stones as large as hen's eggs; and a sledge hammer, weighing fourteen pounds, placed over the pipe, would be kept bouncing up and down continuously, It blew with such force that it could not be lighted next to the mouth of the pipe, except by holding a burning brand over it; but when an attempt was made to light it above, some six or eight feet, it burned finely, making a blaze some ten or fifteen feet high and six to eight feet wide. This was by far the strongest flow of gas ever struck here. Owing to the pipes blowing full of sand and gravel, the flow would die down and almost cease, but as soon as the auger would be put down and the pipe cleared out, it would continue as strong as ever." This well, like the others, was abandoned and allowed to fill up. A few days ago the interest caused by later discoveries and a better understand- ing of the value of the find, led to a partial cleaning out of the well, when the same roarirg sounds were heard as the gas forced its way through some thirty feet of mud and water with a pressure estimated at fifteen pounds to the square inch. The gas was lighted and burned freely. Major Powell in his report on the Mineral Resources of the United States, 1885, speaks of the discovery of natural gas in the Territory, and says: " The gas was found in a vein of gravel, five feet thick and 140 feet below the surface, the pressure being so great as to send up gravel from the bottom of the vein. The gas when lighted showed a blue-green flame, but would only burn when a hot iron rod or burning brand was held over the escape-pipe. The flame reached above five feet in height." RESOURCES 0* DAKOTA. 155 Later, a gas well was struck in the same way, while boring for water, on a farm a mile nearer Blunt, but owing to the proximity of the well to the farm buildings the owner of the property refused to allow it to be fired. The discoveries in this locality, and during the present year, which have led to the organization of a stock company with a capital of $50,000, for the purpose of carrying the gas into the city of Blunt, where it is to be used for heating and lighting the city, and the building up of manufacto- ries, are described by one who has visited the spot and examined the wells, as follows: F 7 " On the 24th of February, while boring for water, Mr. R. M. McClure, living on 23-113-77, Summit township, Sully county, eight miles northwest of Blunt, struck a vein of gas at a depth of 190 feet. A lighted match was applied and it showed signs of force, burning a flame at least four feet high. " Gas not being the object of Mr. Mc( 'lure's search, he pulled out his tubing, abandoned the hole, and proceeded to sink another, about twenty or twenty-five rods north, on a line nearly from his house, in hopes of striking water. At a depth of 194 feet another vein of gas was struck, which appeared to flow freely and with greater force than the first one, and burned with a steady flame. This shafting was also removed, and the hole allowed to fill up with dirt, and no signs of escaping gas can now be noticed. Mr. McClure is perfectly satisfied with the quality, and thinks from the force of the flow that there can be no doubt about the supply. "Mr. Edward Thompson, proprietor of the Blunt roller mills, who ac- companied the writer, while something of a scientist, lays no claims to any special knowledge of the geological formations or science of the earth, yet he questioned closely both Mr. McClure and Mr. Dempsey — the gen- tleman in charge of the drilling machinery — concerning the different strata through which they passed in boring these holes, and it seems just before striking the gas vein that they drilled for a number of feet in a soft slate-stone. There seems to be very little smell to the gas, and what little there is has a tendency toward the fumes of evaporating kerosene. " Going to the hole fiist mentioned, we were informed that it had never been closed; that after its first discovery it was allowed to burn steadily for three weeks, and was used to melt snow for stock and family use, pro- ducing heat sufficient to melt in an hour's time a barrel of water using a large tin pan for a kettle. The snow, however, as it melted in the spring ran down the hole, and it was supposed to be partly filled with water and dirt, yet gas was continually escaping, said Mr. McClure, and a match was lighted, held over the hole, and to our great surprise there came forth a flame of light which carried a feeling of satisfaction with it, substantiating beyond a doubt, every utterance by Mr. McClure." On the 17th of May, Mr. McClure, while continuing his search for water, struck this vein for the third time. The last well, from all reports, is a regular " gusher " — blazing up when fired, to a height of fifteen feet, not- 156 RESOURCES OF DAKOTA. • withstanding the fact that the well is full of slush, and no attempt has ever been made to clean it out. Mr. McClure has since utilized the flow of natural gas in supplying heat for doing the family cooking. The presence of natural gas in any quantity in the vicinity of Fargo, Cass county, was first discovered something over a year ago on the Mon- son farm, eleven miles north, although for a long time previous small flows of gas had been observed in many of the wells dug in that city. During the fall of 1886, a company was formed which built a derrick, im- ported tools from Pennsylvania and sunk a well several hundred feet, in search of the main storage-reservoir of this gas. Cold weather put an end to the operations, but a stock company, lately organized, proposes to con- tinue the well to a depth of 2,000 feet, where it is thought, the heavy vein will be struck. Scientists have made a careful examination of the coun- try, and agree that natural gas probably underlies the entire Red River valley. The flow of the well on the Monson farm has continued unabated for over a year. Within the year past, natural gas was found while sinking an artesian well at Jamestown, Stutsman county. The flow was sufficiently strong to force the gas through 1,300 feet of pipe filled with water, to the surface of the ground where, when lighted, it burned brightly with a flame over a foot in height. This seems to settle the question of the existence of a strong vein of natural gas underlying the James River Valley. A syndi- cate of the most influential and wealthy citizens of Jamestown have or- ganized a stock company with the determination of prosecuting the work of developing natural gas to a profitable end. In sinking wells in the oil fields to the west of the Black Hills a consid- erable flow of natural gas has always been encountered, though no attempt at a systematic investigation has ever been made. It would seem then, that there is no foundation for reasonable doubt of the existence of large bodies of natural gas underlying the Missouri, James, and Red river valleys and the Wyoming coal fields of the Black Hills. The following conclusions by leading scientists as to where natural gas is likely to be found, are of interest. Professor Lesley of Pennsylvania says: " Where the rock formations lie approximately horizontal and have re- mained nearly undisturbed over extensive areas, there is always a chance of finding gas (if not oil) at some depth beneath the surface, deter- mined by the particular formation which appears at the surface. And, wherever rock oil has been found, there and in the surrounding region, rock gas is sure to exist." Professor Orton, state geologist for Ohio, in an elaborate report upon petroleum and inflammable gas, says that there is nothing to establish a rule that natural burning gas can be found only in the neighborhood of RESOURCES OF DAKOTA. 157 deposits of petroleum, and he cites the wells of Indiana, located entirely without the oil belt. Professor Orton lays down a rule of three condi- tions needful to the formation of a natural reservoir containing gas, viz.: A range of highly porous rock, through which the gas traverses, as through pipes; a large fissure into which it flows, and a cap, or lid of im- pervious rock or clay, which will prevent its escape from the reservoir. The Trenton, Berean and Magnesian limestone formations have furnished the first two conditions in Pennsylvania, Ohio and Indiana. Other rocks may furnish it for other regions. The cap, or lid, is sometimes of shale, sometimes of dense, impervious limestone. The professor disproves the theory that natural gas is a product of the natural distillation of petro- leum, but insists that the forces which make natural gas are at work universally, and therefore natural gas can be found almost everywhere. With a discovery of an extended area of natural gas; inexhaustible coal fields, mines of tin, lead, copper, iron, nickel, gold, silver, and other minerals useful to the manufacturer; with flax to supply any number of tow and oil mills; with wheat for countless flour mills; marble, granite, and all the valuable building stones, to be quarried, hewn and polished; vegetables for the. canning factories; with the live stock interests to build up creameries, dairies, cheese factories, pork and beef packing es- tablishments, it is apparent that no other country in the world, offers as great inducements for the safe and profitable investment of capital in the development of mineral wealth and the erection of manufactories, as is presented today, in this wonderland of Dakota. MARBLE, GRANITE, SANDSTONE, QUARTZITE, JASPER, ETC. At Sioux Falls, Dell Rapids and other points of southeastern Dakota, along the Big Sioux river, there is an out-cropping of the most remarkable deposit of quartzite (granite or jasper) ever discovered on the Continent. At Sioux Falls, nearly eighty feet of the rock is exposed and, at Dell Bapids, the perpendicular cliffs of quartzite on either bank of the Sioux river tower to a height of sixty feet above the stream. Some idea of the inexhaustible quantities of this beautiful and useful mineral ma}- be gained from the report of Major Powell, on the United States Geological Surveys, 18S3-4; who estimates the thickness of the deposit to be no less than 3,000 to 4,000 feet, It is said by mineralogists to be equal to the finest granite quarried in Scotland. The texture and color vary somewhat, though generally of a reddish or flesh color, and exceedingly tine-grained. The stone polishes beautifully, taking a glass-like surface, and is as hard, almost, as a diamond — a sharp fragment of the jasper cutting glass with the ease of a glazier's jewel. The J. H. Drake company, (which discovered the commercial value of this beautiful stone, and invented the elaborate and powerful machinery necessary to work it,) has invested 880,000, at Sioux Falls, in a plant for polishing the stone, and a large number of skilled mechanics are em- 158 RESOURCES OF DAKOTA. ployed in the manufacture of elegant designs of ornamental and monu- mental work, which are shipped to all parts of the country. Recently, this company has added to its industry, the working into various shapes, and the polishing of chalcedony, (wood brought from'a petrified forest in Arizona Territory,) being the only firm in the world which has succeeded in the undertaking. The working of these quarries forms a leading industry of Sioux Falls, Ives, and Dell Rapids, and hundreds of men are engaged in the work of chipping the granite into shape for paving blocks, which go to Omaha, to Chicago, and other Eastern cities, and the dressing of building stone which is used in the finest structures at home and abroad. The pay-roll of a single concern, operating quarries at these points, amounts to $24,000 each month. Eight hundred car-loads of this granite were shipped last year, from the city of Dell Rapids alone. In the " Mineral Resources of the United States, 1885," we find the fol- lowing notice of the Sioux Falls quartzite : "This stone is susceptible of a very high polish, and is found in a variety of pleasing tints, such as chocolate, brownish red, brick red, and yellowish. "The polished material has been sold to the amount of $15,000 duringthe last two years," (a trade which has increased wonderfully during the two years since the above was written,) " and polishing works, run by water power, have been erected, and so ingeniously are they contrived that pil- lars, pilasters, mantels, and table tops can be made here as cheaply as anywhere. The pilasters of the German- American bank, in Saint Paul, Minnesota, and the columns in the doorway of the Chamber of Commerce building in the same city, are of this beautiful jasper. It is likely to become one of our choicest ornamental stones, especially effec- tive in combination with the Minnesota red granite. Its great tensile strength, its high, almost mirror-like polish, the'fact that though so high- ly polished, the stone is not slippery, the large pieces that can be quarried out, and the pleasing variety of colors, all combine to render this one of the most desirable building stones. Polishing mills have been built of sufficient capacity to polish $100,000 worth per annum, and in view of the unequaled facility with which it can be prepared for use, it can be made into tablets, blocks, columns, and tiles to advantage, and employed for fine interior and monumental work or in the more artistic branches of stone work." In the Black Hills are found extensive deposits of marble, sandstone, and other valuable and ornamental building stones, of fine texture and great beauty of color. These are described more at length in the article on the "Mineral Resources of the Black Hills," contained in the following pages of this publication. Beds of lime and sandstone are found in a few scattered localities out- si ie of the Black Hills, but in rather limited quantities. However, RESOURCES OF DAKOTA. 159 enough, stone for -walls, foundations, and the usual requirements of build- ing can be had in nearly every county of the Territory. Where no regu- lar deposit of stone is to be found — boulders, broken up by heavy sledges are employed, and make a good wall. OIL. It is reported that petroleum has been discovered in the Turtle Moun- tains region, lying in Rolette county, on the northern boundary of the Territory. "While the report lacks verification, there is little doubt of the existence of oil there, and, because of the rapid settlement now going on in that hitherto undeveloped region, important discoveries of hidden wealth may be looked for. The surfaces of the springs at the foot of the mountains have always been covered over with a scum of oil — a piece of paper saturated in which would ignite quickly, and burn with the fierce flame plainly indicating its properties. Oil, in considerable quantities, has been discovered on the western slope of the Black Hills — in Wyoming, and is used even now, in fact, for lubricating the heavy machinery of the mining districts. It only needs time to demonstrate the presence of oil beneath the sur- face of Dakota — sufficient perhaps, for all demands of home consumption. COAL. The whole country west of the Missouri river and a large part of the surface of north Dakota is underlaid with a deposit of lignite coal, which crops out in many places in veins sometimes twenty feet in thickness. This lignite, or brown coal, is of soft variety, excellent for heating purposes, and has been tested and found to possess gas-making qualities, superior to almost any coal discovered on the Continent. It is denned by mineralo- gists to be one of the most recent geological formations, Post Tertiary, more recent than the anthracite or bituminous coal of the Carboniferous period. It retains, to a great extent, the texture of the wood from which it was formed; and, in mining lignite, vegetable matters are often met with in various stages of their conversion into mineral coal. Sometimes it is more altered in structure, so that its vegetable character is more indistinct; the beds presenting stratified bodies of dark, nearly black substance, with a concoidal fracture. Deposits of lignite occur in many localities of the United States outside of Dakota, notably at Brandon, Vt., Virginia, Texas, Kansas, Oregon, Wyoming, Washington Territory, California, as well as in some of the countries of Europe. The proportion of carbon in this variety of coal is found to vary, by different analyses, from fifty to seventy per cent. To Mr. C. W. Thompson, of Bismarck, who has had a lengthy experi- ence in the mining and handling of Dakota coal, this office is indebted for the following analysis of the lignite found in the Territory: 160 RESOURCES OF DAKOTA. Moisture 12.1 Fixed carbon 58.5 Volatile 27.0 Ash 2.4 Total 100.0 Specific gravity 1.30 While inferior to anthracite, or the best qualities of bituminous coal, lignite burns readily and lurnishes the settlers of a prairie country with that inestimable boon, cheap domestic fuel. At present, because of the lack of transportation facilities, only the outcroppings are worked, and, generally, for the supply simply of the settlers of the immediate neighbor- hood." The completion of the north and south roads already in course of construction, will place the immense coal fields of the northern part of the Territory within easy reach of every village; — and a good quality of soft coal can then be had as low at $2 per ton, — and even in the more dis- tant towns, not exceeding $4.50 per ton. Already, along the Northern Pa- cific railway at Sims, in Morton county, Dickinson, in Stark county, and Little Missouri, in Billings county, coal mining is carried on quite exten- sively and thousands of tons are shipped as far east as Jamestown. It is estimated that during the past winter, ten thousand tons were shipped into the city of Bismarck alone, where it is retailed for §53.50, after paying a tribute of $1 per ton to the only railway line thus far reaching into the coal fields. Recent railroad developments will result, at an early day, in opening to market the extensive coal areas surrounding the Devils Lake, Turtle Mountains, and Mouse river countries, as also of McLean, Mercer, and Emmons counties which contain some of the richest deposits of coal, yet found, but are too distant from present railway facilities. On the north, south, and west of the Black Hills are hundreds of thous- ands of acres of coal in veins of from five to twenty feet in thickness, en- tirely undeveloped, owing to the distance from railways and the cost of transportation. In Day county, in the YYessington Hills, at Plankinton, at Huron, at Yankton, and many other localities of south Dakota there are every indications of the existence of good veins of coal, at a greater or less distance beneath the surface. The great Sioux Indian reservation will undoubtedly prove to be one of the richest coal fields of the Territory, when Congress shall have opened the lands to settlement, which will per- mit of a systematic and scientific investigation of the mineral resources hidden away there. It is authoritatively reported that during the winter season the Indians bring in and sell to the settlers in the vicinity of Scranton and LeBeau, in Walworth county, coal from the Moreau river, in this reservation, which fully equals in quality the best grade of Pennsyl- vania anthracite. An observing writer has said with great truthfulness, that if the people of Dakota were compelled to rely on the home supply for fuel, they would find beneath the surface, everywhere, millions of tons i02 v iong, | [" MAP showing the known COAL AREA of DAKOTA. Drawn for the Commissioner of Immigration, by C. If. Thompson, Bismarck, I). T. June 10th, 1887, -^.Carman j A Du frost Glenboro > Gretna fr \JEro erson ^ . °J7anKaft ^^sJPtefcM ;s f m i - g a v a l ■ e R f Sf n w w. Uow ,~ • * ^ Gertrude J\Thoma3* / jt- Rf^a* ^"iirr- cShs^ji -£eJd b Y ; «*? : ReVeoldfV >t< ^C 5 *- ** • STUTSMAN UM _^ asr -^ i o port I/OGAN ^ MOU\RE^ ^7 E&hleyi _ ununm* - SliSftT PINE S&*~ si: -MTmiffSflla' fc^. - lELJ e MC PHERSON i Hillsvicw