A century of science in America : $b with special reference to the American Journal of Science, 1818-1918
History
A century of science in America : $b with special reference to the American Journal of Science, 1818-1918
American journal of science; Science -- United States -- History
Faith in Noah’s flood as the dominant agent of erosion rapidly lost
ground through the teaching of Lyell after 1830, but the theory of
systematic development of landscapes by rivers gained little. In fact,
Scrope in 1830,[11] in showing that the entrenched meanders of the
Moselle prove gradual progressive stream work, was in advance of his
English contemporary. Judged by contributions to the Journal, Lyell’s
teaching served to standardize American opinion of earth sculpture
somewhat as follows: The ocean is the great valley maker, but rivers
also make them; the position of valleys is determined by original or
renewed surface inequalities or by faulting; exceptional
occurrences—earthquakes, bursting of lakes, upheavals and
depressions—have played an important part. Hayes (1839)[12] thought that
the surface of New York was essentially an upraised sea-bottom modified
by erosion of waves and ocean currents. Sedgwick (1838)[13] considered
high-lying lake basins proof of valleys which were shaped under the sea.
Many of the valleys in the Chilian Cordillera were thought by Darwin
(1844) to have been the work of waves and tides, and water gaps are
ascribed to currents “bursting through the range at those points where
the strata have been least inclined and the height consequently is
less.” Speaking of the magnificent stream-cut canyons of the Blue
Mountains of New South Wales, gorges which lead to narrow exits through
monoclines, Darwin says: “To attribute these hollows to alluvial action
would be preposterous.”[14]
Public-domain text, read in full here on John Shaqi.
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