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Flagg's The Far West, 1836-1837, part 2; and De Smet's Letters and Sketches, 1841-1842

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LETTER IV

Eau Sucree,163 14th July, 1841.

Very Rev. and Dear Father Provincial:

Already two long months have elapsed since we began our journey; but we are at length in sight of those dear mountains that have so long been the object of our desires.164 They are called Rocky, because they are almost entirely formed of granite and silex, or flint stone. The length, position, and elevation of this truly wonderful chain of mountains, have induced geographers to give to it the appellation of "the back-bone of the western hemisphere." Traversing almost the whole of North America, from north to south, containing the sources of some of the largest streams of the world, this chain has for its branches, towards the west, "the spur of the Cordilleras," which divide the Empire of Mexico, and towards the east the less known but not less wonderful mountains of the Wind River, where are found the sources of the large streams that empty themselves into the Pacific and Atlantic Oceans. The Black Hills and the table lands called Prairie hills, which separate the sources of the upper Missouri from those of the Mississippi, the Ozark and the Masserne ridges may all be considered as so many collateral chains of the Rocky Mountains.

According to trigonometrical calculations, and observations, made by means of the barometer, Mr. Boneville,165 in his Memoirs, asserts that the summits of some of these mountains are 25,000 feet high.166 This height would appear much exaggerated, if we consulted only the testimony of the eyes, but it is well known that the mountains which are found in immense plains, are not unlike ships seen on the ocean; they appear much less elevated than they are in reality. Whatever may be the height of these colossal mountains, it was at their base that we hoped to meet our dear neophytes. But a messenger we had sent to acquaint them with our arrival, has just returned, and informed us that the Indians who lay encamped there, about a fortnight ago, went in a southerly direction to hunt the buffalo. We know not whether those Indians were Flat Heads or belong to another nation, and it is to obtain information on this subject, that we are going to despatch a second messenger. In the mean time, I shall continue my journal. The numerous notes, which, on account of our slow progress, we have been enabled to take on the spot, will warrant that exactness of description, which is the more desirable, as it is a quality frequently wanting in the accounts given of these distant regions. Not to exceed the bounds of a lengthy letter, I shall say but little concerning perspectives, flowers, birds, animals, Indians, and adventures.

With the exception of the mounds which run parallel to each other on both sides of the Platte river, and after passing under the Black Hills, disappear at the base of the Rocky Mountains, the whole plain which we traversed for 1500 miles after we had left Westport, might be called the Prairie Ocean. In fact, nearly the whole of this territory is of an undulating form, and the undulations resemble the billows of the sea when agitated by the storm. On the tops of some of these elevations we have seen shells and petrifactions, such as are found on several mountains in Europe. No doubt, some impartial geologists may discover here, as they have done elsewhere, incontestible proofs of the deluge. A petrified fragment which I have in my possession, seems to contain a number of these shells.

In proportion as one removes from the banks of the Missouri or penetrates into the Western regions, the forests lose much in height, density and depth, in consequence of the scarcity of water. Soon after, only the rivers are lined with narrow skirts of wood, in which are seldom seen any lofty creeks. In the neighborhood of creeks and rivulets we generally find willow bushes, and where there is no water it would be vain to look for any thing but grass, and even this grass is only found in the fertile plains that lie between Westport and the Platte river.

This intimate connexion between rivers and forests is so striking to the eye, that our beasts of burden had not journeyed more than eight days through this desert, when we saw them in some manner exult and double their pace at the sight of the trees that appeared at a distance. This was chiefly observable when the day's journey had been rather long. This scarcity of wood in the western regions, so much at variance with what is seen in other parts of North America, proceeds from two principal causes. In the plains on this side of Platte river, from the custom which the Indians who live here have adopted, to fire their prairies towards the end of autumn, in order to have better pasture at the return of spring; but in the Far West, where the Indians do not follow this practice, (because they fear to drive away the animals that are necessary for their subsistence, or to expose themselves to be discovered by the strolling parties of their enemies,) it proceeds from the nature of the soil, which being a mixture of sand and light earth, is every where so very barren that with the exception of the absynth167 that covers the plains, and the gloomy verdure that shades the mountains, vegetation is confined to the vicinity of rivers, – a circumstance which renders a journey through the Far West extremely long and tedious.

At considerable distances, chiefly between the Kants [Kansas] and the Platte rivers, are found blocks of granite of different sizes and colors. The reddish is the most common. In some of the stony parts of the Black Hills are also seen numberless quantities of small pebbles of all shades. I have seen some that were united into solid masses. If these were well polished they would present the appearance of fine mosaics. The columns of the House of Representatives in Washington are deemed very handsome, and are made of similar concretions.

On the feast of St. Peter a remarkable occurrence took place. We discovered an equally curious quarry, which, at first, we took for white marble, but we soon found it something more valuable. Astonished at the facility with which we could fashion this kind of stone into any shape, most of the travellers made calumets of it. I had several made myself, with the intention of offering them as presents to the Indians, so that for the space of forty-eight hours our camp was filled with lapidaries. But the greater number of these calumets could not withstand the action of the fire, and broke. It was alabaster.

The first rock which we saw, and which truly deserves the name, was the famous Rock Independence. It is of the same nature as the Rocky Mountains. At first I was led to believe that it had received this pompous name from its isolated situation and the solidity of its basis; but I was afterwards told that it was called so because the first travellers who thought of giving it a name, arrived at it on the very day when the people of the United States celebrate the anniversary of their emancipation from Great Britain. We reached this spot on the day that immediately succeeds this celebration. We had in our company a young Englishman, as jealous of the honor of his nation as the Americans; hence we had a double reason not to cry hurra for Independence. Still, on the following day, lest it might be said that we passed this lofty monument of the desert with indifference, we cut our names on the south side of the rock, under initials (I. H. S.) which we would wish to see engraved on every spot. On account of all these names, and of the dates that accompany them, as well as of the hieroglyphics of Indian warriors, I have surnamed this Rock "the Great Record of the Desert." I shall add a few remarks about the mounds that are seen in the vicinity of the Platte river. The most remarkable of all, at least that which is best known to the generality of travellers, is the mound to which they have given the name of "chimney." It is called so on account of its extraordinary form; but instead of applying to it an appellation which is rather unworthy this wonder of nature, just because it bears some resemblance to the object after which it is named, it would have been more proper to call it "the inverted funnel," as there is no object which it resembles more. Its whole height, including the base, body and column, is scarce less than four or five hundred feet; the column or chimney is only about one hundred and thirty feet high, so that there is nothing striking in the loftiness of its dimensions. But what excites our astonishment, is the manner in which this remnant of a mountain, composed of sand and clay, has been so shaped, and how it has for such a length of time preserved this form, in spite of the winds that are so violent in these parts. It is true that this mound, and all those that are found near it, is composed of a successive number of horizontal and perpendicular strata, and has about the middle a zone or belt, consisting of a vein of petrified clay. If from these two facts it would be inferred that at a certain height the substance of which the horizontal and perpendicular strata are formed, is susceptible of being hardened so as to approach the nature of stone, then we might perhaps account in some manner for the wonderful formation of this curious ornament. Yet the main difficulty would still remain, and we would at last be compelled to have recourse to the system of occult qualities. The existence of the chimney is therefore a problem, and if any scientific person should wish to solve it, I would advise him to repair to this monument without delay, as a cleft which is seen at the top, and which in all probability will soon extend to the base, threatens to leave nothing of it but the remembrance of its existence.168

 

The chimney is not the only remarkable mound to be met with in this vast solitude. There are many others of various forms. One is called "the House," another "the Castle," a third "the Fort," &c. And, in fact, if a traveller was not convinced that he journeys through a desert, where no other dwellings exist but the tents put up at night and removed in the morning, he would be induced to believe them so many ancient fortresses or Gothic castles and with a little imagination, based upon some historical knowledge, he might think himself transported amid the ancient mansions of Knight errantry. On one side are seen large ditches, and high walls; on the other, avenues, gardens and orchards; farther on, parks, ponds, and lofty trees. Sometimes the fancy presents a castle of the middle ages, and even conjures up the lord of the manor; but instead of all these magnificent remains of antiquity, we find only barren mounds on all sides, filled with cliffs formed by the falling of the waters, and serving as dens to an infinite number of rattle snakes and other venomous reptiles.169

After the Missouri, which in the Far West is what the Mississippi is in the North, the finest rivers are the Kanzas, the Platte, and the Eau Sucree. The first of these falls into the Missouri, and receives the waters of a great number of tributary streams. Of these tributaries we counted as many as eighteen before we reached the Platte. Hence we may infer that the country abounds in springs, and that the soil is compact and covered with verdure. The reverse may be said of the neighborhood of the Platte, where springs and verdure are seldom seen. Even on the mounds that run parallel to its banks, the waters that fall from the clouds, upon a sandy and porous soil, run down into the vallies. But the prairies that receive the overflowing waters of the river are extremely fertile, and appear beautiful in spring, being enamelled with a great variety of flowers. The sight of the river itself is still more pleasing; though in spite of all its beauties, it has, like the most remarkable of its mounds, received a vulgar name. This proceeds from the custom which some travellers have of applying to objects the names of things with which they are well acquainted. They have called it Platte or Flat river, on account of its width and shallowness; the former often extending six thousand feet, whilst its depth is but from three to five feet, and sometimes less. This want of proportion destroys its utility. Canoes cannot be used to ascend it, and if barges sometimes come down from Fort La Ramee to the mouth, it is because they are so constructed that they may be converted into sledges and pushed on by the hands of men. The author of Astoria has properly defined it "the most magnificent and most useless of rivers." Abstraction made of its defects, nothing can be more pleasing than the perspective which it presents to the eye; though besides the prairie flowers and the ranunculus, its banks bear only the eglantine and the wild vine; for on account of the fires made in the autumn the lofty vegetation is entirely confined to the islands that stud its surface. These islands are so numerous that they have the appearance of a labyrinth of groves floating on the waters. Their extraordinary position gives an air of youth and beauty to the whole scene. If to this be added the undulations of the river, the waving of the verdure, the alternations of light and shade, the succession of these islands varying in form and beauty, and the purity of the atmosphere, some idea may be formed of the pleasing sensations which the traveller experiences on beholding a scene that seems to have started into existence fresh from the hands of the creator. Fine weather is common in this temperate climate. However, it happens sometimes, though but seldom, that the clouds floating with great rapidity open currents of air so violent, as suddenly to chill the atmosphere and produce the most destructive hail storms. I have seen some hailstones of the size of an egg. It is dangerous to be abroad during these storms. A Sheyenne Indian was lately struck by a hailstone, and remained senseless for an hour. Once as the storm was raging near us, we witnessed a sublime sight. A spiral abyss seemed to be suddenly formed in the air. The clouds followed each other into it with such velocity, that they attracted all objects around them, whilst such clouds as were too large and too far distant to feel its influence turned in an opposite direction. The noise we heard in the air was like that of a tempest. On beholding the conflict we fancied that all the winds had been let loose from the four points of the compass. It is very probable that if it had approached much nearer, the whole caravan would have made an ascension into the clouds, but the Power that confines the sea to its boundaries and said – "Hitherto shalt thou come," watched over our preservation. The spiral column moved majestically towards the North, and alighted on the surface of the Platte. Then, another scene was exhibited to our view. The waters, agitated by its powerful action, began to turn round with frightful noise, and were suddenly drawn up to the clouds in a spiral form. The column appeared to measure a mile in height; and such was the violence of the winds which came down in a perpendicular direction, that in the twinkling of an eye the trees were torn and uprooted, and their boughs scattered in every direction.170 But what is violent does not last. After a few minutes, the frightful visitation ceased. The column, not being able to sustain the weight at its base was dissolved almost as quickly as it had been formed. Soon after the sun re-appeared: all was calm and we pursued our journey. In proportion as we proceeded towards the sources of this wonderful river, the shades of vegetation became more gloomy, and the brows of the mountains more cragged. Every thing seemed to wear the aspect, not of decay, but of age, or rather of venerable antiquity. Our joy was extatic as we sung the following Ode composed for the occasion:

 
Non ce n'est plus une ombre vaine,
Mes yeux ont vu, j'en suis certain,
Dans l'azur d'un brilliant lointain,
Des Monts Rocheux la haute chaine, &c.
 
 
O! no – it is no shadow vain,
That greets my sight – yon lofty chain
That pierces the ethereal blue;
The Rocky Mounts appear in view.
 
 
I've seen the spotless, virgin snow,
Glist'ning like gems upon their brow —
And o'er yon giant peak now streams
The golden light of day's first beams.
 
 
How from their ice-clad summits, steep,
The living waters joyous leap!
And gently on thro' vallies gay,
Sweeter than honey wend their way.
 
 
It is because on yon proud height,
The standard floats of life and light:
It is, that there th' Omnipotent
Hath pitched His everlasting tent —
The God whose love no tongue can tell,
Among his children deigns to dwell.
 
 
All hail! majestic Rock – the home
Where many a wand'rer yet shall come;
Where God himself, from His own heart
Shall health and peace and joy impart.
 
 
Sorrow adieu – farewell to fear, —
The sweet-voiced hymn of peace I hear;
Its tone hath touched the red-man's soul:
Lo! o'er his dark breast tear-drops roll.
 
 
O! soon the silent wilderness
Shall echo with his song of praise;
And infant lips, from morn till ev'n,
Shall chaunt thy love – great King of heav'n.
 
 
Father and God! how far above
All human thought, Thy wondrous love!
How strange the path by which Thy hand
Would lead the Tribes of this bleak land,
From darkness, crime and misery,
To live and reign in bliss with Thee!
 

As I have been speaking of rivers I shall give (you) a short geographical description of the Missouri, which I am inclined to call my river, as I have so often ascended and descended it during the last four years, travelled along its banks, and crossed almost all its tributaries from the mouth of the Yellow Stone to the place where the mighty river mingles its turbid stream with that of the peaceful Mississippi. I have drunk the limpid waters of its sources, and the muddy waters at its mouth, distant more than three thousand miles from each other. The prodigious length of its course, the wildness and impetuosity of its current have induced the Scioux to call it "the furious." Whenever I crossed this magnificent river the sensations which I experienced bordered on the sublime, and my imagination transported me through the world of prairies which it fertilises, to the colossal mountains whence it issues. It is in the heart of the Rocky Mountains that the Missouri takes its rise, together with many other magnificent streams; such as "the Father of Waters," into whose bosom it flows, after having fertilised its own borders to a vast extent, – the Arkansas, and the Red river, both, like itself, majestic tributaries; the Columbia, which becomes the reservoir of all the waters of the Oregon territory, and the Rio Colorado which after winding its course through a gloomy and rocky desert, invigorates the most beautiful part of California. The Missouri, properly so called, is formed by three considerable forks that unite their waters at the entrance of one of the passes of the Rocky mountains. The North fork is called "the Jackson," the South "the Gallatin," and the one between them "the Madison."171 Each one of these is subdivided into several small arms that flow from the mountains, and almost mingle their waters with those of the upper forks of the Columbia on the western side. I have drunk of both, distant only about fifty yards from each other; for the same field of snow supplies both the Atlantic and Pacific oceans. After the junction of the forks, the Missouri for a considerable distance, becomes an impetuous and foaming torrent. Below this, its bed is more spacious, and its course more tranquil. Steep rocks of a black hue jut and rise above its current to a height of nearly a thousand feet. The mountains, along whose base it runs, are shaded by pines, cedars, fir and turpentine trees. Some of these mountains present a solitary aspect, and wear a look of unspeakable grandeur. The river, for the space of seventeen miles, is seen raging and foaming, rolling from cataract to cataract with a roaring noise that is repeated by all the neighboring echoes. The first of these cataracts measures ninety-eight feet in height; the second, nineteen; the third, forty-seven, and the fourth, twenty-six. Below the Falls, the beautiful river of Mary,172 flowing from the North, adds its peaceful waters to those of the rapid and impetuous stream. Still lower, but on the opposite side, the Dearborn and the Fancy disembogue themselves through mouths respectively 150 feet in width.173 After many other rivers of considerable width and extent, we come to the Yellow Stone, the largest but one of all the tributaries of the Missouri, and resembling the latter in many respects. This river too has its source in the Rocky Mountains, and is 850 yards wide at its mouth; its bed is spacious, its current rapid; its length is about 1600 miles, and at its confluence with the Missouri it appears to be the larger of the two. For a considerable distance above the mouth its banks are well wooded, and its bottom lands are extensive and very fertile.174 The grey and black bear, the big horn, the antelope, the stag and the common deer frequent these regions, whilst coal and iron mines are in such abundance that for 50 years they might supply fuel and materials to a countless number of steam engines.

 

After the Missouri has received the Yellow Stone river, its bottom lands become more extensive; yet as little or no wood is found on them, it may be long before attempts will be made to cultivate them. The White Earth river coming from the North, and the Goose river from the South, are not very considerable. The width of each at the mouth is 300 yards. The Little Missouri, though shallow, has a rapid current, and has its sources in the South, as also the following streams:175 Cane river, near the village of the Mandans; Cannon Ball river, Winnipenhu, Sewarzena and Sheyenne river, which is navigable for 400 miles; a rapid and muddy stream, 400 yards at the mouth;176 Teton river and White river, so called on account of the color of its waters, which are unwholesome. It is navigable for 300 miles, has a rapid current, and measures about 300 yards at its mouth. The lands which it waters in the upper country are barren, and abound in animal and vegetable petrifactions, whilst its banks have every where a fantastic appearance.177 Next and on the same side we meet the Poncas and Running Water river, the latter of which has a fine current. Medicine and Jacques rivers enter the Missouri from the opposite side; the latter is also called the rendezvous of the beaver hunters and runs nearly parallel with the Missouri.178 After the White Stone and the Vermillion, we find the Big Scioux river, on which is found the fine red stone quarry explored by the Indians to make their calumets. The Floyd and the Roger, the Maringoin, the Nishnebatlana and the Nedowa fall into the Missouri on the Northern side.179 Its chief tributary, the Platte, rises like itself in the Rocky Mountains and extends its course nearly two thousand miles. Though it be a mile wide at the mouth yet it is shallow, as its name indicates, and is not navigable, the two Nemahas flow from the South and the Little Platte from the North.180 The Kanzas, on the South side, is about a thousand miles long, and is navigable to a great distance. Grand river, from the North, is a wide, deep and navigable stream. The two Charetons are found on the same side, whilst the Osage and Gasconade rivers enter from the South. The former is an important stream, navigable for 600 miles, and having its sources near the waters of the Arkansas; whilst the latter, though navigable only for 66 miles, is equally important, on account of the fine large pine forests that supply St. Louis and the adjacent country with lumber. I shall say nothing of the many other less remarkable tributaries of the Missouri, such as the Blue Water, the Mine, the Bonne Femme, the Manitoo, the Muddy, the Loutre, the Cedar, the Buffalo, the St. Johns, the Wood river, the Charette, Bonhomme, Femme Osage, &c.181 The length of the Missouri, from its sources to the Yellow Stone, is 880 miles, from the Yellow Stone to its junction with the Mississippi, is about 2200. I subjoin a list of the Forks of its great tributaries which I have seen and crossed.

Beaver Head, Big Hole Fork, Stinking Water, Forks of the Jefferson, Powder River, Tongue River, Rose-bud River, Big Horn River, Clarke River, Rocky River, Traverse River, Loutre River, 25 Yard River, Gallatin River, Wind River, Forks of the Yellow Stone. Horn River, Wolf River, Bigwood River, North Fork River, South Fork River, Cabin Pole River, Horse River, La Ramee, Eau Sucree, Forks of the Platte. Grande Sableuse, Horse Shoe River, St. Peter's River, Red River, Kennion River, Deer River, The Torrent, Branches of the North Fork of the Platte. Soldier's River, Ouaggerehoosse River, Vermillion River, Black Vermillion River, Sick River, Knife River, Blue Waters, Forks of the Kanzas. Mary's River, Big Bone, Yungar River, Potatoes River, Grand Fork, Forks of the Osage.

I left off my narrative on Sugar River, otherwise called Eau Sucree; I must interrupt it to listen to the good tidings that are brought from the mountains.

I remain, Rev. and Dear Father,
Your dutiful Son in Christ,
P. J. De Smet, S.J.
163Sweetwater River, for which see Wyeth's Oregon, in our volume xxi, p. 53, note 33. – Ed.
164The route followed from the point where the trail reached the Platte, was along the river to its forks, thence up the South Fork to its ford, across to the North Fork at Ash Creek, along the south bank of the former stream to the junction of the Laramie, thence continuing by the North Fork to its crossing, near the present Caspar, Wyoming, and along the north bank, across country to the Sweetwater, to avoid the cañon of the North Platte. – Ed.
165For a brief sketch of Captain Bonneville, see our volume xx, p. 267, note 167. – Ed.
166The highest peaks of the Rocky Mountains, and of the whole Cordilleran system within the boundaries of the United States, do not much exceed fourteen thousand feet. – Ed.
167The sage-brush (Artemisia tridentata), the European species of which is known as wormwood or absinth (A. absinthium). See ante, p. 174, note . – Ed.
168Bidwell thus describes this landmark: "A noted landmark on the North Fork, which we sighted fifty miles away, was Chimney Rock. It was then nearly square, and I think it must have been fifty feet higher than now, though after we passed it a portion fell off." Century Magazine, xix, p. 118. – Ed.
169See engravings of these fantastically cut rocks in Century Magazine, op. cit., p. 121. – Ed.
170Bidwell mentions both the cyclone with its destructive hail, and the water-spout which passed a quarter of a mile behind the camp. – Ed.
171The three forks of the Missouri were named by Lewis and Clark (1805) in honor of the president of the United States and his chief advisers, the secretaries of state and of the treasury. – Ed.
172Maria's River, for which see our volume xxiii, p. 84, note 73. – Ed.
173Dearborn River, named by Lewis and Clark (1805) for the secretary of war, was in reality a western affluent above, not below, the Great Falls. By "Fancy," De Smet probably intends the stream named by Lewis and Clark "Tansy," but now known as Teton River – a tributary, however, of Maria's River, although approaching very near the Missouri. – Ed.
174For the "Yellowstone" see our volume xxii, p. 375, note 351. – Ed.
175On these streams see Maximilian's Travels, in our volume xxii, pp. 367, 368, 369, notes 342, 344, 345. – Ed.
176For these rivers consult the following: Cane (Knife), our volume xxii, p. 357, note 333; Cannonball, ibid., p. 338, note 306; Winnipenhu (Grand), our volume xxiv, p. 87, note 59; Sewarzena (Moreau), our volume v, p. 127, note 82; Cheyenne, ibid., p. 126, note 81. – Ed.
177For Teton River, South Dakota, see our volume xxiv, p. 45, note 26; for White River and its "bad lands," ibid., p. 90, note 64. – Ed.
178For Ponca Creek see our volume xxii, p. 291, note 253; the Niobrara (Running Water) is noted in our volume v, p. 90, note 54; the James (Jacques), in volume xxii, p. 282, note 238. Medicine is a small creek in northeastern Nebraska. – Ed.
179Whitestone is the name given by Lewis and Clark to the stream afterwards known as the Vermilion – see our volume vi, p. 87, note 31; for the Big Sioux see ibid., p. 85, note 30; Floyd's Creek comes in just below the bluff of the same name, where Sergeant Charles Floyd of the Lewis and Clark expedition was buried – see our volume v, p. 91, note 56; the Boyer (Roger) is noted in our volume xxiv, p. 105, note 83; the Maringoin is probably intended for the Moingoina (Des Moines), a western tributary of the Mississippi; see our volume vi, p. 73, note 24, for the Nishnabotna; and v, p. 37, note 5, for the Nodaway (Nedowa). – Ed.
180For the Nemaha see our volume vi, p. 72, note 23; the Little Platte rises in Union County, southern Iowa, and flows southward through that part of Missouri known as the Platte purchase. – Ed.
181These are all Missouri streams, mentioned for the most part by Lewis and Clark (see Original Journals, index). Upon Wood River (Du Bois) the expedition rendezvoused during the winter of 1803-04. – Ed.