riassFg^J? FRKHKN'TEI) IW ^4i§!p©l?^ ®f @i|MHD p©i|K§ (;©(3Hf^. WHlj Special I^efewnce TO THE First tgn veftRS * ^ OF e*e ^ GRftND FORKS CITY, e/V^ <\^/^ Iqcluding aq l-(islorica! Oulline nhmh ,L^- er-^ Of ^^e F(ed F^iv'er Valiey, BY H. V. ARNOLD. Labimobe: Pjoneek Office. 1900. si^^HD p®i|i^§ (^©o^ifp^. 09if}? gpGcial I^efej'ence TO THE FiF$ IRST TeN YeftRS * « OF ^ * GRftND FORKS CITY. ^M/\\v I p^E^^ I ^V^ qcluding aq |-(isiorical Oulline^ '-^ ^^^ Q|: 11^^ i^^j 1^1^^^ Valley. BY h: vfARNOLD. II Larimore: Pioneer Office. 1900. A? A7 GOVERNMENT TOWNSHIP. N GIFT AUTHOR '95 PREFATORY REMARKS. rpHE history of the Red River Valley, so far as it has been published in _L this state, appears to have been confined to newspaper, magazine and other sketches. The next step is special pamphlets, and finally will come the bound books of the future. No really good history of the valley which will in- clude the era of the settlements, can be written until some progress has been made in collecting facts of that character concerning each of the counties of the Red River tier. The history of that part of the valley south of the inter- national boundary is chiefly confined to its North Dakota side, which, in- deed, is the best portion of it in United States territory. The current of its history, however, also includes a strip of territory along the Minnesota side of Red River and which extends from Georgetown to Breckenridge. But the North Dakota side of the valley is specially historic ground, particularly its northern boundary around Pembina and Walhalla. Any work, even in pamphlet form, purporting to be a history of any one of the counties of the Red River tier of North Dakota, must necessarily sift over the accumulating records that belong to the history of the yalley in its entirety, for unless this be done, its old phase of life, the sequence of events and their bearing on the commencement of the modern epoch cannot be duly appreciated. The present is the outgrowth of past conditions; no hiatus, no abrupt transition separated the old phase of life in the valley from the com- mencement of the present civilization. Yet with the beginning of the latter account has to be taken of the great migration which has rendered this civil- ization a possibility. For a century past we have before us a rather contin- uous historic stream in the Northwest with which white men have been concerned. At present the literature bearing upon this subject, is in a rather discord- ant state, unsifted, and more or less filled with erroneous statements of fact, including discrepant and wrong dates. These sketches merely supply a tem- porary want. It would, perhaps, be a mistake to imagine that any permanent harm has been done in the matter of these errors; on the contrary, the dis- crepancies being apparent to anyone of critical intelligence, the outcome will be to stimulate others to investigate the facts they handle more carefully, so as to eliminate and correct the mistakes of their predecessors in the same field, also bringing to light other and new facts. A valuable series of articles on "Old Times in the Red River Valley," writ- ten by M. H. Morrill, were published in the Richland County Gazette in 1897 and '98; during the first half of 1898 another valuable series entitled "The Long Ago" collected by Chas. H. Lee, editor of the Walhalla Mountaineer, appeared in his paper and were subsequently issued in pamphlet form. More recently, the Grand Forks Herald in a notable illustrated 40-page edition of June 27, 1899, commemorating its twentieth anniversary, was rich in respect to its historical contributions and which were remarkable for their accuracy. The Record Magazine, of Fargo, formerly edited by C. A. I^ounsberry, and more recently by W. F. Gushing, begun in May, 1895, has also since that date gathered a large fund of valuable historical and descriptive matter concern- ing the Red River Valley and state of North Dakota. Doubtless the files of the Northwest Magazine of St. Paul, contain many articles of similar character. Numerous brief historical sketches concerning the city of Grand Forks were formerly included in special editions of the city papers and were also used in a few other Avorks. The earlier history of Grand Forks has never been more than merely skimmed over, no atteinpt ever having been made in these publications to treat the subject in detail. The original nucleus of these sketches appears to have been an historical article that appeared in a large illustrated edition of the Plaindealer for Christmas week. 1890, if, indeed, it was not older. It is observable that the style and subject matter of that sketch has tinctured all subsequent writings upon the subject. There was an historical sketch covering much the same ground and which appeared in the first number of the weekly Herald In June, 1879, but that of the Plain- dealer appears to have been an independent production. The later sketches, although more or less amplified, as manipulated by different hands, all bear the stamp of the original exemplar. IV PREFATORY REM ARKS Portions of the present work have been clipped from articles by the writer that have appeared in the Larimore Pioneer during the last several years, the parts here retained having undergone more or less revision. In treating of the historical outline of the Red River Valley the earlier numbers ot the Record Magazine have occasionally been drawn upon for the basis of some of the facts narrated. As in the case of some other writers dealing with valley history, fragments from other sources have been now and then interwoven with the basis to round out paragraphs in respect to additional details, where these are not of the nature of extracts. In respect to the county history, much of it has been based upon the direct testimony of the Old Settlers, although contemporary records, always the best historical evidence, have been used so far as these have been obtainable. - Although great care has been exercised by the author in eliminating errors of statement and particularly erroneous dates from the materials used, it would be too much to claim that this work can be faultless in these respects. But whatever accuracy that portion of it may possess which bears upon the early history of the county and the city of Grand Forks, is due to the kindly help of the Old Settlers of the Red River Valley whose contributiou of facts are acknowledged either in footnotes or by name in the text, though innumer- able other points derived from them and others are inwrought into the various paragraphs of the last three parts of this work. In making these acknow- ledgments of assistance from others, we should also mention John Nelson, Register of Deeds of this county, in assisting us in an examination of the old- est records of his office: also W. P. Davies, city editor of the Grand Forks Herald, through whose courtesy we were enabled to look through the oldest bound file of that paper. The author himself has been a resident of the county since May, 1880, and considerable matter has been incorporated in this work derived from his own personal knowledge and observations. Moreover, for many years past, much information covering innumerable points of local history, "has also been derived from persons resident in and around Larimore. The inferences that have been drawn from any special fact, or group of facts, or comments on the same, are generally the thoughts of the writer. i<:hrata. Page 1.— The figures for the 96th and 97th meridians should read 97th and 98th meridians. The error resulted from a slip of memory. Page 2.— The breadth of the fiat valley plain on the main line of the Great NortLern Railway is at least thirteen miles wide. While the ten mile limit may be taken as a geological boundary, it is none the less certain that the district between the Elk Valley and Red River flats constitutes a distinct topographical land-belt of the county, although this may merge impercept- ably with the valley plain. This correction also correspondingly modifies the stated breadth of this central land belt. See Note A, p. 127. Page 11.— Altitude of Kempton, 1126 feet, should read 1127 feet. Page 13.— "Comparative few Indians." The first of these words should read Comparatively. Page 103.— E. O. Steelman, now a resident of Elm Grove township, states that he was of the party who emigrated from Minnesota to Turtle river in June, 1878, but arrived at Grrand Forks about ten days later than the others. H. A. Morgan came through with a team of horses the next fall. Edward Wheeler, it seems, was not an original settler, but bought out the claim or right of a colored man named James Hawarden. Pages 106 and 107.— The names of certain settlers of Inkster and Strabane townships given as Casey, Congrave and McEwen should have been spelled Corey, Congram and McElwain. Mr. Inkster states that he removed to the Mouse River country in August, 1882, and not in 1885. See Note H. P^^K,T I. DESCRIPTIVE SKETCH. GENEKAT. DESOKIPTION POSITION AND BOUNDARIES. HE NORTH jind south row of counties, six in number, tlmt border the enstern side of the ut.'ife of North Djikotii, constitute wiiat is called its "Ked Kiver tier." (irjind Forks county occu- pies nearly a midway position in this row, being: fourth in order from tlie south. The county is bounded north by Wsilsh, east by Red river which alwo forms the dividing line be- tween INiinnesota and North J^akota, south by 'I'raill and Steele, and west by Nelson county. The 48th pariillel of latitude crosses the county about four miles to the north of its medial line, and its area is almost wholly included between the 96th and 97th meridians. DIMENSIONS AND AREA. 'I'he county has an average length of -10 miles from east to west, yet there is a difference of about twelve miles between the length of its southern and northern boundary lines, whicli is chiefly due to the westerly trend of Ked river where this stream flows abreast of the county. The south line toucliing Traill and Steele counties has a westward extension of about 47 miles from ttie river; an miles. The county is divided into 42 townships, thirty-six of which correspond with the surveyor's or government townships, the remaining ones be- ing those that border on lied river, or ihe parts of the congres- sional townships accruing to tho county by being bisected by this stream. The county contains 921,000 acres, or 1,440 square miles. This is a little more than (he total land area of the little state of l{hod(» Island. Tf I ^< T () R ^■ () F G R AND FORKS CO F N T Y TOPOGRAPHY AND DRAINAGE. The Imiidreds of counties in the Union dider widely in respect to ilieir topoj^rnphy or surface features. Their surfaces vary from those that lie broadly level to those that are mountainous in their physical aspect. The presence of lakes, river valleys, outcropping ledges of rock, forests and wooded hills, creates variety in the scenery and beautifies the landscape. In this county the differences in altitude are such as to have caused very marked changes in the form of the surface were these elevations converged nearer together so as to have given rise to steep hill sides or abrupt declivities; but this is not the case here. The surface of Grand Forks county is partially level and par- tially rolling, but, on the whole, has a graduiif ascent from the riv- er to the height of the upland country, the surface being more prominent in tracts of successively higher elev;ition than any otiier form. A line drawn from the city of Grand Forks across the center of the county to its western verge would cross four separate land belts, or districts in which somewhat different top- ographical coiiditions exist. First and- lowest comes the Red r.ver flats, a level prairie plain next to the river, and which ex- tends outward about ten miles on this line. Second in order, there occurs the midway slope of the main valley, a gradually ascending and gently rolling tract of about sixteen miles in width. 'I'he third land belt is the "Elk Valley," a level prairie district that is four miles wide on the line now under consideration. J.MStly there comes the upland country, a district more rolling than hilly, which, within ihe county limits, is eight miles across on its medial line. Toward the southern border of tlie county the form of the sur- face is nearly similar to that just described .''or its incdial line, but with these viiriations: A narrower width to the fiat valley plain, a greater breadth to both the midway slope and the Elk Valley, and the inclusion of a wider portion of the upland coun- try within the county limits. In the northern part of the county, along its north tier of town- ships, the lay of the land varies a little from that already de- scribed. Here the flats extend somewhat farther west than in the southern half of the county; then a long, but slight ascent of the surface toward the west occurs, with an occasional slight ridge, until west of Inkster the latid further rises in a consider- able ridge; between this elevation and the uplands there is a shallow valley (the northern extension of the Elk Valley) and west of this the uolands rise to their usual height, their aftitude being nearly uniform through the west part of the county, but the breadth of this hill distri-^^t in this part of the county is less than the distance across a township. C; E N E R A L D E y f II I P T I () N ,'J On the whole, the surfnce of the county is mainly of the nature of a gradual or very <>entle rise westward from Red river, attain- ing a height of over 600 feet in forty miles. It is not exact to state that the county is a vast level plain. lUit such ascent as exists, is Dot an uniformly smooth rise; were it so, this would only av- erage fifteen or sixteen feet to the mile. Some of the slopes are several times greater than this, hut no very rough features exist in the county. 'I'he lowest land is presumably in 'I'urtle Kiver township; the highest in the county is some one of the elevated swells of the uplands, the extreme variation in altitude not be- ing f.ir from 050 feet. i'he topogrnphy of any countycliiefly determines its drainage directions. The drainage of Grand Forks county is chiefly fruin the uplands to Red river east by north, but with vaiiations from this direction in some parts of it. The central part is drained by Turtle river, a small stream with several smaller afttuents. To the north of the Turtle the slope of the land is more directly to- ward the east than the course of the stream itself,, but in the northern part of the county, within a limited area, the drain- age slope is northward to Forest river. Tliis stieam is mainlv confined within the limits of Walsh county, but its upper reaches intersect Inkster and Strabane townships of this county. li\ the eastern part the drainage is b')th northerly to the 'I'urtle and east to lied river. In its southwestern part, the drain;ige is Irom the uplands toward the southeast or by way of (Joose river, the principal stream of 'J'raill county. On the eastern slope ot the uplands, the drainnge lines are in the form of coulees, or narrow, winding ravines, some of which ai-e several miles in length, fifteen or twenty rods wide, and forty or fifty feet det^p, but dry through most of the year, though they sometimes contain through the summer pool-* and little trickling streams. Tfiere are a few small streams in the county, mere rills or brooks, which, after flowing several miles, disappear in the ground by absorption of the water, or in other cases, enter small ponds or marshes without permanent outlets. The flowage of streams jn this part of tlie Northwest is consid- erably less tiiitn would otherwise be the case, were the country largely covereii with lorests and underlaid by stiata, of bedrock atamodeiate depth from the surface, neither of which factors are present here. But these facts have their bearing on the cultiv- able area ol the county, there beirjg lio great amount of waste latid in it, resulting either from thickets, miirshes or hilly tracts. THE VALLEY PLAIN. The valley plain forms a very extensive belt of level prairie land lying next to tJie river, and, in this county, it extends out- ward eight to twelve miles distant fronj the stream. The "Pied 4 II I S T O 1? Y O F O E A N D F O R K S C O r; X T Y Kiver flats," as tliese lands are sometimes cilled, correspond to tlie alluvial bottom lands of niany bluff hemmed western rivers, which usually have much less width thnn the IJed Iiiver V^alley. The land has a slight rise toward the west, iwo to ihree or more feet to the mile, or sufficient to insure drainnge and prevent the flat hind becoming a morass. 'IMie streams crossing it flow mere- ly in chajinels sunk fifteen to twenty feet below the common prairie level. The altitude of Grjind Forks is 8oO leet above sea-level, and taking into consideration the slight westward as- cent of this land and the northward descent of the valley of .'lbou^ one foot to the mile, the average elevation of thnt j);irtofthe valley plain comprised in this county would range about ten feet higher than the site of Grand Forks. 'i'his hind has a deep and rich alluvial soil entirely free from stone. "Th'^ lied river has cut a channel twenty to fifty feet deep. It is bordered by only few and narrow areas of bottom land, instead «)f which its banks usually rise steeply on one side and by mod- erate slopes on the other to the lacustrine plain, which thence reaches nearly level ten to thirty miles from the river."* A very nmrked feature of the northwestern country is the tim- ber belts that fringe the banks of the larger ctrGams and to a considerable extent those of their tributaries. Helts of timber line both banks of Red river, following in a sort of zisr-zag or sinuous course, the windings of the stream, but as seen across country from a distance of several miles, it appears to form in- stead a dark band against the horizon that trends away to the north and south in nearly a straight course. This is all the more distinct in winter by contrast with the snow clad valley jilain. There are points in the county, where, from the higher land, the timl)er belt along Red river can be discerned at a distance of twenty to thirty miles, THE MIDWAY SLOPE. There is a broad belt of bowlder clay land running north and south, or bearing a little northwest and s ..utheast, Through the middle part of the county. It comprises the gentle slope of the Red River valley between the Klk Valley and uplands on the west, Jind the valley plain on the east. 'I'his land belt also ex- tends through Traill and W'alsh counties, and where it is trans- versely crossed by any of the tributaries of Red river, they flow in consideiable sized valleys containing timbered bottom Ian Is of limited extent, and as the streams have no very small amount of fall while crossing this belt, they have many rapids in bowl- der strewn channels, with occasional reaches of slack water. I'o the south of Turtle river, this district is gently undulating, or *The (ilacial Lake .\gassiz, by Warren I'pham, ]\Innoarapli of the rnite^l States (Jeoloaioal Smvey. Washington, isa=s. ii. I'O. G E X E U A L D i: S (Mi I P T I O X 5 characterized by low, broad ridges. Between Larimore and Ojata and on the line of the Great Xorthern Railway, the descent of this slopii anionnts to abont 275 feet. The western 1,000 feet coiitonr line of the lied Kiver Valley passes throngh this county along this slope between Emerado and Arvilla, sind within one niile^of the latter place. It approaches nearer to the river in the southern part of the county, and recedes nioie awny from it to the north of its central part. This land belt has a sandy, but fertile surface loam and bowlder clay subsoil. Its western por- tion is 1,100 feet above sea-level. THE ELK VALLEY. Persons living at a distance, and who are unfamiliar with this part of the county, are apt to suppose from its designation that the Elk N'^alley i^ the basin of some stream. h'rom McCanna south to CJoose river this land belt is more of the nature of a bench, or second prairie level of the main valley slope thiin an actual valley, since between the points named, it is bordere H I S' TOR Y O F (J R A N D PO R K S COUNT V a mile wide and from 75 to 100 feet deep, along a distance of 1| mile. In Walsh county the long", shallow depressi.)n between this ridge and the uplands is called the Golden Valley. As confined to Walsh county, it varies (rom 4^ to one mile in breadth, being contracted to this lesser distance at one point toward its north- ern termination. From the north branch of Forest river it has a northern extension of eighteen miles, and from the same point southward, so far as anything of the nature of a valley exists, it has a farther length of about sixteen miles. This sixteen mile stretch may properly be called the Elk Vallev. Its southerly continuation through Grand* Forks county and overlap into 'i'raill county, covers a distance of S5 miles, and as stated, this portion of the tract is of the nature of a second prairie level, not being enclosed on the east bv any prominent rise cf ground. As mapped out, this portion of the land belt is in the form of an elongated key-stone, or of an estuary to a river, and varies from four or five to ten or twelve miles in Jjreadth. This part IS called by Warren Upham, "The Delta of ihe Flk Valley." This IS in relation to its geological formation. The most of this tract forms a level prairie belt along the base of the uplands which, at l.arimore, is four miles wide. Tiiere is but litile rise of the level part of this land belt toward the uplands and what ascent exists is confined to a fringe of territorv a mile in breadth along their base. As a geological unity the whole tract, valley and prairie, has a total length of about 70 miles, with a very sliirht ascending slope from south to north, which is the reverse of that of the main valley. This is shown by the fact that iMayville and Port- land m the neighborhood of the southern ternnnation of this delta deposit have an altitude of 978 and 983 feet respectively while the northern end of the Golden Valley is about 1 200 feet above the sea, and intermediate points have a gradually in- creasing elevation northward. Around Larimore the land' has an average altitude of 1,130 feet, with variations of a iew feet above and below this level. The soil of the Flk Valley is a fertile, sandy clay loam the percentage of sand contained in it being of a fine sort rather than coarse grained. The subsoil is a sandy bed of clay but this IS not everywhere present. J.ike the soil of the valley plain, that of the Flk \ alley is free from bowlders, and more ponms. THE WESTERN ESCARPMENT. The western side Of the Red River Vallev in North Dakota and the Canadian provinces is bordered by a notable escarp- ment, much more conspicuous than the correspondiuir one on the eastern side of the valley. That on the west forms^ a second GENERAL D E S C K I I' T I O N 7 and for some portions of the v.illey, a third prairie level, wliicli is the Ciise in tliis county. This escarpment is separated at intervals by the entrnnce into the Red liiver Valley of streams from the west, vvhich in turn have wide valleys. These separat- ed portions of the common escarpment bear specific names, as Pembina, Riding and Duck mountains. Along the upper por- tion of the valley from Lake Traverse northward for about one Jjundred miles, this escarpment is low, possessing only a niod- erntely Jiscending slope, but farther north, and also in the Can- adian Dominion, its height increases, both above Red river and sea-level. Toward Lake Traverse the altitude above sea-level is about 1,200 feet, gradually increasing to 1,500 feet in the Pem- bina mountains, and towering to an elevation of 2,700 feet to the west of l^ake Winnipeg. From the head of the Coteau des Prairies north to Pembina county, this escarpment bears no specific name, being called sometimes the 'uplands," but more commonly the "hills." This escarpment forms the western verge of the ifJed River Valley. Its height forms a gently rolling upland country of a wid«^ area, extending westward toward J)evils lake. Belv/een Jiarimore and Devils Lake city, the surface nowhere exceeds an altitude of 1,585 feet on the railroad line. The hill country, within the limits of Grand Forks county, is commonly stated to have an elevation of oOO feet above the l^^lk Valley, and has about the same altitude within the limit just specified, as that of the village ot Niagara, which is 1,440 feet above sea-level. Some of the swells of the surface are likely to be more elevated. The comparatively small portion of the upland country wllliin the limits of this county, constitutes about one-sixth of the area of said county. There are practically five of its townships thstt are included in its hill district, and alsf) parts of several others. The soil is a gravelly clay loam of decomposed glacial drift, well mixed with organic matter, and makes fairly fertile land. (ie