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 — John Shaqi
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
On embarking in the morning, the wind was slightly ahead, which
continued during the forenoon, changing in the after-part of the day, so
that we were able to hoist sail. About four o'clock the weather became
cloudy and hazy, the wind increasing, at the same time attended with
thunder and lightning. A storm was rapidly gathering, and the lake
became so much agitated that we immediately effected a landing, which
was not done without some difficulty, on a shallow and dangerous shore,
thickly strewn with boulders. We pitched our tents on a small peninsula,
or narrow neck of land, covered with beautiful forest-trees, which was
nearly separated from the main shore. Shortly after our arrival a vessel
hove in sight, and anchored on the same dangerous lee shore. We were in
momently expectation of her being driven from her moorings, but were
happily relieved, the next morning, to observe that she had rode out the
storm.
The lake was still too rough on the following day, and the wind too
high, to permit our embarking. We made an excursion inland. The country
proved low, undulatory, and swampy. The forest consisted of hemlock,
birch, ash, oak, and maple, with several species of mosses, which gave
it a cold, bleak character. The margin of the forest was skirted with
the bulrush, briza canadensis, and other aquatic plants. The whole day
passed, a night, and another day, with nothing but the loud sounding
lake roar in our ears. A heavy bed of the erratic block formation
commences at this point, and continues to Point aux Barques, the eastern
cape of Saganaw Bay.
In one of these displaced masses--a boulder of mica slate, I discovered
well-defined crystals of staurotide. This formed my second mineralogical
acquisition.[17] There were, also, some striking water-worn masses of
granitical and hornblende porphyry.
[17] In passing along this coast in 1824, an Indian picked up, in
shallow water, a small boulder imbedding a mass of native silver.
Breaking off the most prominent mass, he still observed the metal
forming veins in the rock, and brought both specimens to an officer of
the British Indian department at Amherst (Lieut. Lewis S. Johnson),
who presented them to me. This discovery is described in the _Annals
of the New York Lyceum of Natural History_, vol. i. part 8, page 247.
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