Questions of geography and astronomy may deserve a moment's attention. If we assume the discovery of the mouth of the Mississippi to have been made by Narvaez in 1527--a doubtful point!--a period of 305 years has elapsed before its actual source has been fixed. If the date of De Soto's journey (1541) be taken, which is undisputed, this period is reduced to 290 years. Hennepin saw it as high as the mouth of the river St. Francis in 1680. Lt. Pike, under the administration of Mr. Jefferson, ascended it by water in 1805, near to the entrance of Elk River, south of the Crow Wing Fork, and being overtaken at this spot by frosts and snow, and winter setting in strongly, he afterwards ascended its banks, on snow shoes, his men carrying his baggage on hand sleds, to Sandy Lake, then a post of the North-west Company. From this point he was carried forward, under their auspices, by the Canadian train de-glis, drawn by dogs to Leech Lake; and eventually, by the same conveyance, to what is now denominated Cass Lake, or upper Lac Cedre Rogue. This he reached in January, 1806, and it formed the terminus of his journey.
In 1820, Gen. Cass visited Sandy Lake, by the way of Lake Superior, with a strong party, and exploratory outfit, under the authority of the government. He encamped the bulk of his party at Sandy Lake, depositing all his heavy supplies, and fitted out a light party in two canoes, to trace up the river to its source. After ascending to the point of land at the entrance of Turtle River into Cass Lake, it was found, from Indian accounts, that he could not ascend higher in the state of the water with his heavy canoes, if, indeed, his supplies or the time at his command would have permitted him to accomplish it, compatibly with other objects of his instructions. This, therefore, constituted the terminal point of his journey.
The length of the river, from the Gulf of Mexico to Itasca Lake, has been estimated at 3,160 miles. Barometrical observations show its altitude, above the same point, to be 1,680 feet--which denotes an average descent of a fraction over six inches per mile.
The latitude of Itasca Lake has been accurately determined to be 47° 13' 35"--which is nearly two degrees south of the position assigned to it by the best geographers in 1783, the date of the definite treaty of peace between the United States and Great Britain.
The reason of this geographical mistake has been satisfactorily shown in traversing up the stream from the summit of the Pemidjegomag, or Cross-water Lake--during which, the general course of the ascent is due south.
CHAPTER XLIV.
Descent of the Mississippi River, from Itasca Lake to Cass Lake--Traits of its bank--Kabika Falls--Upsetting of a canoe--River descends by steps, and through narrow rocky passes--Portage to the source of the Crow-Wing River--Moss Lake--Shiba Lake--Leech Lake--Warpool Lake--Long Lake Mountain portage--Kaginogomanug--Vermilion Lake--Ossawa Lake-Shell River--Leaf River--Long Prairie River--Kioskk, or Gull River--Arrival at its mouth--Descent to the Falls of St. Anthony, and St. Peter's--Return to St. Mary's.
1832, July 14th. I found the outlet of Itasca Lake to be about twelve feet wide, and some twelve to fourteen inches deep. The water is of crystal purity, and the current very rapid. We were urged along with great velocity. It required incessant vigilance on the part of the men to prevent our frail vessels from being dashed against boulders. For about twelve miles the channel was not only narrow, but exceedingly crooked. Often, where the water was most deep and rapid, it did not appear to exceed ten feet in width. Trees which had fallen from the banks required, sometimes, to be cut away to allow the canoes to pass, and it required unceasing vigilance to avoid piles of drifted wood or boulders. As we were borne along in vessels of bark, not more than one-eighth of an inch thick, a failure to fend off, or hit the proper guiding point, in any one place, would have been fraught with instant destruction. And we sat in a perfect excitement during this distance. The stream then deployed, for a distance of some eight miles, into a savannah or plain, with narrow grassy borders in which its width was doubled, its depth decreased, and the current less furious. We went through these windings with more assurance and composure. It was one of the minor plateaux in which this stream descends. The channel then narrowed and deepened itself for another plunge, and soon brought us to the top of the Kabika Palls. This pass, as the name imports, is a cascade over rocks. The river is pent up, between opposing trap rock, which are not over ten feet apart. Its depth is about four feet, and velocity perfectly furious. It is not impossible to descend it, as there is no abrupt pitch, but such a trial would seem next to madness. We made a portage with our canoes of about a quarter of a mile across a peninsula, and embarked again at the foot of the falls, where the stream again expands to more than double its former width, and the scenery assumes a milder aspect. It is another plateau.
Daylight had departed when we encamped on a high sandy bank on the left shore. We were perfectly exhausted with labor, and the thrilling excitement of the day. It seemed, while flying through its furious passes, as if this stream was impatient for its development, and, like an unrestrained youth, was bent on overthrowing every obstacle, on the instant, that opposed its advance and expansion. A war horse could not have been more impatient to rush on to his destiny.