A Book of the United States. Various

in a region of lakes, upon the table-lands, which throw their waters north into Hudson’s Bay—south into the gulf of Mexico—and east into the gulf of St. Lawrence—it pursues its course to the falls of Peckagama, a distance of two hundred and thirty miles, through a low prairie, covered with wild rice, rushes, sword grass, and other aquatic plants. During this distance, it is extremely devious as to course and width, sometimes expanding into small lakes, at others, narrowing into a channel of about eighty feet. It is about sixty feet wide on its exit from Red Cedar or Cassina Lake, with an average depth of two feet; but from the junction of the Leech Lake fork, increases to a hundred feet in width, with a corresponding increase of depth. Its current, during this distance is still and gentle; and its mean velocity may be estimated at a mile and a half per hour, with a descent of three inches per mile. This is the favorite resort of water-fowl, and amphibious quadrupeds.

      ‘At the falls of Peckagama, the first rock stratum, and the first wooded island, is seen. Here the river has a fall of twenty feet; and from this to the falls of St. Anthony, a distance of six hundred and eighty-five miles, exhibits its second characteristic division. At the head of the falls of Peckagama, the prairies entirely cease; and below, a forest of elm, maple, birch, oak, and ash, overshadows the stream. The black walnut is first seen below Sandy Lake river, and the sycamore below the river De Corbeau. The river, in this distance, has innumerable well wooded islands, and receives a number of tributaries, the largest of which is the river De Corbeau, its great south-western fork. The Pine, Elk, Sac, and Crow rivers, also enter on the west, and the St. Francis and Missisawgaiegon, on the east. The course of the river, although serpentine, is less so, than above the falls of Peckagama, and its bends are not so short and abrupt. Its mean width may be estimated at three hundred feet until the junction of the De Corbeau, and below that at two hundred and fifty yards. Its navigation is impeded, agreeably to a memorandum which I have kept, by thirty-five rapids, nineteen ripples, and two minor falls, called the Little and the Big Falls, in all of which the river has an aggregate descent of two hundred and twenty-four feet in fourteen thousand six hundred and forty yards, or about eight miles. The mean fall of the current, exclusive of the rapids, may be computed at six inches per mile, and its velocity at three miles per hour. In the course of this distance it receives several small turbid streams, and acquires a brownish hue, but still preserves its transparency, and is palatable drink-water. A few miles above the river Corbeau, on the east side, we observe the first dry prairies, or natural meadows, and they continue to the falls of St. Anthony. These prairies are the great resort of the buffalo, elk, and deer, and are the only parts of the banks of the Mississippi where the buffalo is now to be found. Granite rocks appear at several of the rapids, in rolled pieces, and in beds; and in some places attain an elevation of one or two hundred feet above the level of the water, but the banks of the river are generally alluvial.

      ‘At the falls of St. Anthony, the river has a perpendicular pitch of forty feet, and from this to its junction with the Missouri, a distance of eight hundred and forty-three miles, it is bounded by limestone bluffs, which attain various elevations from one to four hundred feet, and present a succession of the most sublime and picturesque views. This forms the third characteristic change of the Mississippi. The river prairies cease, and the rocky bluffs commence precisely at the falls of St. Anthony. Nine miles below it receives the St. Peter’s from the west, and is successively swelled on that side by the Ocano, Iowa, Turkey, Desmoines, and Salt rivers, and on the east by the St. Croix, Chippeway, Black, Ouisconsin, Rock, and Illinois. One hundred miles below the falls of St. Anthony, the river expands into a lake, called Pepin, which is twenty-four miles long and four in width. It is, on issuing from this lake, that the river first exhibits, in a striking manner, those extensive and moving sandbars, innumerable islands and channels, and drifts and snags, which continue to characterize it to the ocean. Its bends from this point onward are larger, and its course more direct; and although its waters are adulterated by several dark colored and turbid streams, it may still be considered transparent. The principal impediments to navigation in this distance are the Desmoines, and Rock river rapids. The latter extends six miles, and opposes an effectual barrier to steam-boat navigation, although keel-boats and barges of the largest classes, may ascend. This rapid is three hundred and ninety miles above St. Louis.

      ‘The fourth change in the physical aspect of this river is at the junction of the Missouri, and this is a total and complete one, the character of the Mississippi being entirely lost in that of the Missouri. The latter is, in fact, much the larger stream of the two, and carries its characteristic appearances to the ocean. It should also have carried the name, but its exploration took place too long after the course of the Mississippi had been perpetuated in the written geography of the country, to render an alteration in this respect, either practicable or expedient. The waters of the Mississippi at its confluence with the Missouri, are moderately clear, and of a greenish hue. The Missouri is turbid and opake, of a grayish white color, and during its floods, which happen twice a year, communicates, almost instantaneously, to the combined stream its predominating qualities, but towards the close of the summer season, when it is at its lowest stage of water, the streams do not fully incorporate for twenty or thirty miles, but preserve opposite sides of the river; and I have observed this phenomenon at the town of Herculaneum, forty-eight miles below the junction.

      ‘The water in this part of the river cannot be drank until it has been set aside to allow the mud to settle. The distance from the mouth of the Missouri to the gulf of Mexico is one thousand two hundred and twenty miles, in the course of which it receives from the west, the Merrimac, St. Francis, White, Arkansas, and Red rivers; and from the east, the Kaskaskia, Great Muddy, Ohio, Wolf, and Yazoo. This part of the river is more particularly characterized by snags and sawyers, falling-in banks and islands, sand-bars and mud-banks; and a channel which is shifting by every flood, and of such extreme velocity, that it was formerly thought it could not be navigated by vessels propelled with sails. Subsequent experience has shown this conjecture to be unfounded, although a strong wind is required for its ascent. It is daily navigated in ships of from four hundred to eight hundred tons burden, from the Balize to New Orleans, a distance of one hundred miles, and could be ascended higher were it necessary; but the commerce of the river above New Orleans is now carried on, in a great measure, by steam-boats. The width of the river opposite St. Louis is one mile; it is somewhat less at New Orleans, and still less at its disembochure. A bar at its mouth prevents ships drawing more than eighteen feet water from entering. This river is occupied by different bands of the Chippeway Indians from its sources, to the Buffalo Plains in the vicinity of the upper St. Francis, the precise limit being a matter of dispute, and the cause of the long war between them and the Sioux. The Sioux bands claim from thence to the Prairie des Chiens, and the Foxes and Sacs to the river Desmoines. From this vicinity to the gulf of Mexico the Indian title has been extinguished by the United States’ government, either through purchase, treaty, or conquest, and we have now the complete control of this river and all its tributary streams, with the exception of the upper part of Red river. The wild rice is not found on the waters of the Mississippi south of the forty-first degree of north latitude, nor the Indian reed, or cane, north of the thirty-eighth. These two productions characterize the extremes of this river. It has been observed by McKenzie, that the former is hardly known, or at least does not come to maturity, north of the fiftieth degree of north latitude. The alligator is first seen below the junction of the Arkansas. The paroquet is found as far north as the mouth of the Illinois, and flocks have occasionally been seen as high as Chicago. The name of this river is derived from the Algonquin language, one of the original tongues of our continent, which is now spoken nearly in its primeval purity by the different bands of Chippeways.’

      The navigation upon this river is very great. Ships seldom ascend higher than Natchez. It is navigable for boats of the largest size as far as the Ohio. The number of steam-boats upon the Mississippi is about three hundred. Their size is from five hundred and forty tons downwards. The passage from Cincinnati to New Orleans and back has been made in nineteen days. From New Orleans to Louisville the shortest passage has been eight days and two hours, the distance being one thousand six hundred and fifty miles, and against the current. The steam-boats have generally high-pressure power, and many fatal explosions have happened upon these waters. The first steam-vessel here was built in 1810.5

      The Missouri rises in the Rocky Mountains in nearly the same parallel with the Mississippi, and about a mile distant from the head-waters