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
The mode of this formation may be clearly seen. Winds, at some ancient
period, have been the agent of blowing the sands, as they were washed up
by the lake, and redepositing them on part of a prostrated forest,
resting directly on the clay stratum. The trees, thus buried in dry
sand, have been preserved. In process of time, the river encroached upon
these antique beds, exposing them to view. There are also antique
fresh-water shells found in similar positions near this spot. No rock
is, thus far, found _in sitû_ in ascending the lakes. The old surface of
the country is wholly of diluvial formation, except where it shows lake
action.
HURON COAST FROM FORT GRATIOT TO MICHILIMACKINAC.--About two hundred and
thirty miles lie stretched out between these two points. Lake Huron
charms the eye, with the view of its freshness and oceanic expanse. But
the entrance is without rock scenery, and the student of its geology
must be a patient gleaner along its shores. Long coasts of sand and
gravel extend before the eye, and they are surmounted, at a moderate
elevation, with a dense foliage, which limits the view of its structure
to a narrow line. Portions of this coast are heavily loaded with the
primitive debris[212] from the North. These are found, in some places,
in heavy masses, but all are more or less abraded, showing that they
have been transported from their original beds. In one of these, I
observed crystals of staurotide.
[212] In 1824, an Indian brought me a specimen of native silver found
on this part of the coast. It was imbedded in a boulder of mixed
granite and steatite.
The first section of this coast reaches from Fort Gratiot to Point aux
Barques, a distance of about seventy-five miles. Nearly midway lies the
White Rock, a very large boulder of whitish-gray semi-crystalline
limestone, lying off the shore about half a mile, in water of about one
and a half fathom's depth. It is the effect of gulls lighting upon this
rock, and not the intensity of the color of the stone, that has
originated the name--which is a translation of the _Roche Blanche_ of
the older _voyageurs_. The Detroit clay-formation still characterizes
the coast.
Public-domain text, read in full here on John Shaqi.
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