Summary Narrative of an Exploratory Expedition to the Sources of the Mississippi River, in 1820: Resumed and Completed, by the Discovery of its Origin in Itasca Lake, in 1832Schoolcraft, Henry Rowe
History
Summary Narrative of an Exploratory Expedition to the Sources of the Mississippi River, in 1820: Resumed and Completed, by the Discovery of its Origin in Itasca Lake, in 1832
Schoolcraft, Henry Rowe
Great Lakes (North America); Mississippi River -- Sources; Northwest, Old -- Description and travel
Bidding adieu to the Leech Lake chief the next morning at sunrise (4 h.
45 m.), after giving him a lancet, with directions to vaccinate any of
his people who had been overlooked, I embarked on the Kaginogamaug. This
is a beautiful lake, with sylvan shores and crystal water, some four or
five miles long. We were just forty minutes, with full paddles, in
passing it. The outlet is narrow, and overhung with alders. The width is
not over six feet, with good depth, but the turns are so sudden, and the
stream so thickly overhung with foliage, that the use of the axe and the
paddle as an excavator were often necessary. It then expands into a
lake, called Little Vermilion, which is fringed with a growth of birch
and aspen, with pines in the distance. Its outlet is fully doubled in
width, and we had henceforth no more embarrassment in descending. This
outlet is pursued about eight miles. I noticed the tamarack on its
banks, and the nymphæ odorata, scirpus lacustris, and Indian reed on the
margin. It expands into Birch Lake, a clear sheet, about one mile long,
with pebbly bottom, interspersed with boulders. A short outlet, in which
we passed a broken fish-dam, connects it with Lac Plè. This lake is
about three and a half miles long, exhibiting a portion of prairie on
its shores, interspersed with small pines. From it, there is a portage
to Ottertail Lake, the eastern source of Red River. This is the common
war road of the Mukundwa against the Sioux.
On coming out of Lac Plè, freshwater shells began to show themselves,
chiefly species of naiades, a feature in the natural history of this
stream which is afterwards common; but I observed none of much size, and
they are often greatly decorticated. Four or five miles lower, we
entered Assowa Lake, and about a mile and a half further, Lac Vieux
Desert, or Old Gardon Lake, so called from the remains of a trading
station, where we halted for breakfast. On resuming the descent, just
twenty minutes were required, with vigorous strokes of the paddle, to
pass it. It has an outlet about two miles long, when the stream again
expands into a lake of considerable size, which we called Summit Lake.
Thus far, we had been passing on a geological plateau of the diluvial
character, extending southwest. But from this point the course of the
river veers, at first towards the east and northeast, and, after a wide
circuit, to the southeast, and eventually again to the southwest. From
this point, rapids begin to mark its channel. The river, consequently,
assumes a velocity which, while it hurries the traveller on, increases
his danger of running his frail bark against rocks or shoals. We had
been driven down this accelerated channel two hours and fifteen minutes,
when it expanded into a sheet called Long Rice Lake. This is some three
miles in length, and, at a very short distance below it, the river again
expands into a considerable lake, which, from the circumstance of Lieut.
Public-domain text, read in full here on John Shaqi.
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