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
The phenomena demanding explanation—jumbled masses of “diluvium,”
polished and striated rock, bowlders distributed with apparent disregard
of topography—were indeed startling. Even Lyell, the great exponent of
uniformitarianism, appears to have lost faith in his theories when
confronted with facts for which known causes seemed inadequate. The
interest aroused is attested by 31 titles in the Journal during its
first two decades, articles which include speculations unsupported by
logic or fact, field observation unaccompanied by explanation, field
observation with fantastic explanation, _ex-cathedra_ pronouncements by
prominent men, sound reasoning from insufficient data, and unclouded
recognition of cause and effect by both obscure and prominent men. With
little knowledge of glaciers, areal geology, or of structure and
composition of drift, all known forces were called in: normal
weathering, catastrophic floods, ocean currents, waves, icebergs,
glaciers, wind, and even depositions from a primordial atmosphere
(Chabier, 1823). Human agencies were not discarded. Speaking of a
granite bowlder at North Salem, New York, described by Cornelius
(1820)[33] as resting on limestone, Finch (1824)[34] says: “it is a
magnificent cromlech and the most ancient and venerable monument which
America possesses.” In the absence of a known cause, catastrophic
agencies seem reasonable.
_The Deluge._
In the seventh volume of the Journal (1824)[35] we read:
“After the production of these regular strata of sand, clay,
limestone, &c. came a terrible irruption of water from the north, or
northwest, which in many places covered the preceding formations with
diluvial gravel, and carried along with it those immense masses of
granite, and the older rocks, which attest to the present day the
destruction and ruin of a former world.”
Another author remarks:
“We find a mantle as it were of sand and gravel indifferently covering
all the solid strata, and evidently derived from some convulsion which
has lacerated and partly broken up those strata....”
The catastrophe favored by most geologists was floods of water violently
released—“we believe,” says the editor, “that all geologists agree in
imputing ... the diluvium to the agency of a deluge at one period or
another.”[36] Such conclusions rested in no small way upon Hayden’s
well-known treatise on surficial deposits (1821),[37] a volume which
deserves a prominent place in American geological literature. Hayden
clearly distinguished the topographic and structural features of the
drift but found an adequate cause in general wide-spread currents which
“flowed impetuously across the whole continent ... from north east to
south west.” In reviewing Hayden’s book Silliman remarks:
Public-domain text, read in full here on John Shaqi.
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