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
Buffon gives two engravings of this animal, as found in Canada, under
separate names; but it is apprehended that he has been misled by the
same animal seen in its summer and winter dress. To the Indian, this
animal is valuable for its quills, which are dyed of bright colors, to
ornament their dresses, moccasons, shot-pouches, and other choice
fabrics of deer skin, or birch bark. This animal has four claws on the
fore paw, and five on the hinder ones. It has small ears hid in the
hair, and a bushy tail, with coarse black and white hair. The specimen
killed would weigh eight pounds.
[33] John Sullivan Pierce (N. H., brother to Colonel Benjamin K.
Pierce), Third Lieutenant Third Artillery, April 5, and Second
Lieutenant, May, 1814; retained, May, 1815, in Artillery; First
Lieutenant, April 1818; resigned February 1, 1823.--_Gardner's Army
Dictionary._
Soon after coming out from this indentation of the lake, we came in
sight of Point Detour, on turning which, from E. to N., we found no
longer use for sails. Mackenzie places this point in north latitude 45°
54´.
The geology of this coast appears manifest. Secondary compact limestone
appears in place, in low situations, on the reef of Outard Island and
Point, and in the approach to Point Detour. A ridge of calcareous
highlands appears on the mainland east of Michilimackinac, stretching
off towards Sault de Ste. Marie, in a northeast direction. This ridge
appears to belong to a low mountain chain, of which the Island of
Michilimackinac may be deemed as one of the geological links. Just
before turning, we passed a very heavy angular block of limestone, much
covered with moss, which could not have been far removed, in the drift
era, from its parent bed. The largest angle of this stone, which I have
since examined, must be eight or ten feet. This block is of the
ortho-cerite stratum of Drummond Island. The shores are heavily charged
with various members of the boulder drift, with a fringe beyond them of
spruce and firs, giving one the idea of a cold, exposed, and most
unfavorable coast. Turning the Point of Detour, we ascended the strait a
few miles, and encamped on its west shore, off Frying-pan Island, at a
point directly opposite the British post of Drummond Island, which we
could not perceive, but the direction of which was clearly denoted by
the sound of the evening bugles.
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