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 essence of physiography is the belief that land forms represent
merely a stage in the orderly development of the earth’s surface
features; that the various dynamic agents perform their characteristic
work throughout all geologic time. The formulation of principle and
processes of earth sculpture was, therefore, impossible on the
hypothesis of a ready-made earth whose features were substantially
unchangeable, except when modified by catastrophic processes. In 1821,
J. W. Wilson wrote in the Journal: “Is it not the best theory of the
earth, that the Creator, in the beginning, at least at the general
deluge, formed it with all its present grand characteristic
features?”[4] If so, a search for causes is futile, and the study of the
work performed by streams and glaciers and wind is unprofitable. The
belief in the Deluge as the one great geological event in the history of
the earth has brought it about that the speculations of Aristotle,
Herodotus, Strabo, and Ovid, and the illustrious Arab, Avicenna
(980–1037), unchecked by appeal to facts but also unopposed by
priesthood or popular prejudice, are nearer to the truth than the
intolerant controversial writings of the intellectual leaders whose
touchstone was orthodoxy. A few thinkers of the sixteenth century
revolted against the interminable repetition of error, and Peter
Severinus (1571) advised his students: “Burn up your books ... buy
yourselves stout shoes, get away to the mountains, search the valleys,
the deserts, the shores of the seas.... In this way and no other will
you arrive at a knowledge of things.” But the thoroughgoing
“diluvialist” who believed that a million species of animals could
occupy a 450–foot Ark, but not that pebbles weathered from rock or that
rivers erode, had no use for his powers of observation.
Sporadic germs of a science of land forms scattered through the
literature of the seventeenth and eighteenth centuries found an
unfavorable environment and produced inconspicuous growths. Even their
sponsors did little to cultivate them. Steno (1631–1687) mildly
suggested that surface sculpturing, particularly on a small scale, is
largely the work of running water, and Guettard (1715–1786), a truly
great mind, grasped the fundamental principles of denudation and
successfully entombed his views as well as his reputation in scores of
books and volumes of cumbrous diffuse writing.
At the beginning of the nineteenth century a sufficient body of
principles had been established to justify the recognition of an earth
science, geology, and the 195 volumes of the Journal thus far published
carry a large part of the material which has won approval for the new
science and given prominence to American thought. From the pages in the
Journal, the progress of geology may be illustrated by tracing the
fluctuation in the development of fact and theory as relates to valleys
and glacial features, the subjects to which this chapter is devoted.
Public-domain text, read in full here on John Shaqi.
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