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
It was stated to us at Michilimackinac, that Lake Huron had fallen one
foot during the last year. It was also added that the decrease in the
lake waters had been noticed for many years, and that there were, in
fact, periodical depressions and refluxes at periods of seven and
fourteen years. A little reflection will, however, render it manifest
that, in a region of country so extensive and thinly populated,
observations must be vaguely made, and that many circumstances may
operate to produce deception with respect to the permanent diminution or
rise of water, as the prevalence of winds, the quantity of rain and snow
which influences these basins, and the periodical distribution of solar
heat. It has already been remarked, while at the mouth of Fox River,
that a fluctuation, resembling a tide, has been improperly thought to
exist there, and, indeed, similar phenomena appear to influence the
Baltic. Philosophers have not been wanting, who have attributed similar
appearances to the ocean itself. "It has been asserted," observed
Cuvier, "that the sea is subject to a continual diminution of its level,
and proofs of this are said to have been observed in some parts of the
shores of the Baltic. Whatever may have been the cause of these
appearances, we certainly know that nothing of the kind has been
observed upon our coast, and, consequently, that there has been no
general lowering of the waters of the ocean. The most ancient seaports
still have their quays and other erections, at the same height above the
level of the sea, as at their first construction. Certain general
movements have been supposed in the sea, from east to west, or in other
directions; but nowhere has any person been able to ascertain their
effects with the least degree of precision."[150]
[150] Theory of the Earth. Modern geologists attribute these changes
to the rising or sinking of the earth from volcanic forces.
Public-domain text, read in full here on John Shaqi.
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