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
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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
We proceeded two leagues, and encamped at Point aux Pins, on the
Canadian shore. At six o'clock the next morning we were again in our
canoes, and crossed the strait, which is here several leagues wide, to
the west, or Point Iroquois Cape. In this traverse we first beheld the
entrance into Lake Superior. The scene is magnificent, and I could fully
subscribe to the remark made by Carver, "that the entrance into Lake
Superior affords one of the most pleasing prospects in the world." The
morning was clear and pleasant, with a favoring breeze, but a tempest of
wind and rain arose, with severe thunder, soon after we had
accomplished the passage, which compelled us hastily to land on the
Point Iroquois shore. This storm detained us five or six hours before
the waters were sufficiently calm to embark. Among the boulders, I
picked up a fine specimen of graphic granite, most perfectly
characterized. About two o'clock, we entered this great inland sea. How
feeble and inadequate are all geographical attempts to describe this
vast body of water, with its imposing headlands, shores, and islands.
The St. Mary's River passes out between two prominent capes, called Gros
Cape and Point Iroquois. The former rises up in elevated barren peaks of
sienite and hornblende rock; the latter consists of nearly equally
elevated masses of horizontal red sandstone, covered with a dense
forest. The line of separation is, perhaps, three leagues, forming a
geological gap, through which, at ancient periods, the drift and boulder
strata has been forced, with an amazing power. For we find these
boulders, of the disrupted sienites, hornblende, trap, and sandstone
rocks of these northern latitudes heaped in profusion along the entire
shores of the river, and cast out, far and wide, into the basin of Lake
Huron.
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