Man and the Glacial PeriodWright, G. Frederick (George Frederick)
History
Man and the Glacial Period
Wright, G. Frederick (George Frederick)
Glacial epoch; Prehistoric peoples
Some of the most remarkable instances of ancient river channels buried
by the glacial deposits have been brought to light in southwestern Ohio,
where there has been great activity in boring for gas and oil. At St.
Paris, Champaign County, for example, in a locality where the surface
of the rock near by was known to be not far below the general level, a
boring was begun and continued to a depth of more than five hundred feet
without reaching rock, or passing out of glacial _débris_.
Many years ago Professor Newberry collected sufficient facts to show that
pretty generally the ancient bed of the Ohio River was as much as 150
feet below that over which it now flows. During a continental elevation
the erosion had proceeded to that extent, and then the channel had been
silted up during the Glacial period with the abundant material carried
down by the streams from the glaciated area. One of the evidences of
the preglacial depth of the channel of the Ohio was brought to light at
Cincinnati, where "gravel and sand have been found to extend to a depth
of over one hundred feet below low-water mark, and the bottom of the
trough has not been reached." In the valley of Mill Creek, also, "in the
suburbs of Cincinnati, gravel and sand were penetrated to the depth of
120 feet below the stream before reaching rock." But from the general
appearance of the channel, Professor J. F. James was led to surmise
that a rock bottom extended all the way across the present channel of
the Ohio, between Price Hill and Ludlow, Ky., a short distance below
Cincinnati, which would preclude the possibility of a preglacial outlet
at the depth disclosed in that direction. Mr. Charles J. Bates (who was
inspector of the masonry for the Cincinnati Southern Railroad while
building the bridge across the Ohio at this point) informs me that Mr.
James's surmise is certainly correct, and that his "in all probability"
may be displaced by "certainly," since the bedded rocks supposed by
Professor James to extend across the river a few feet below its present
bottom were found by the engineers to be in actual existence.
Public-domain text, read in full here on John Shaqi.
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