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
“Passing over to England in the spring of 1805, and fixing my
residence for six months in London, I found there no school, public or
private, for geological instruction, and no association for the
cultivation of the science, which was not even named in the English
universities.” In geology “Edinburgh was then far in advance of
London.... Prof. Jameson having recently returned from the school of
Werner, fully instructed in the doctrines of his illustrious teacher,
was ardently engaged to maintain them, and his eloquent and acute
friend, the late Dr. John Murray, was a powerful auxiliary in the same
cause; both of these philosophers strenuously maintaining the
ascendancy of the aqueous over the igneous agencies, in the geological
phenomena of our planet.
On the other hand, the disciples and friends of Dr. Hutton were not
less active. He died in 1797, and his mantle fell upon Sir James Hall,
who, with Prof. Playfair and Prof. Thomas Hope, maintained with signal
ability, the igneous theory of Hutton. It did not become one who was
still a youth and a novice, to enter the arena of the geological
tournament where such powerful champions waged war; but it was very
interesting to view the combat, well sustained as it was on both
sides, and protracted, without a decisive issue, into a drawn
battle....
The conflicts of the rival schools of Edinburgh—the Neptunists and the
Vulcanists, the Wernerians and the Huttonians, were sustained with
great zeal, energy, talent, and science; they were indeed marked too
decidedly by a partisan spirit, but this very spirit excited untiring
activity in discovering, arranging, and criticising the facts of
geology. It was a transition period between the epoch of geological
hypotheses and dreams, which had passed by, and the era of strict
philosophical induction, in which the geologists of the present day
are trained....
I was a diligent and delighted listener to the discussions of both
schools. Still the igneous philosophers appeared to me to assume more
than had been proved regarding internal heat. In imagination we were
plunged into a fiery Phlegethon, and I was glad to find relief in the
cold bath of the Wernerian ocean, where my predilections inclined me
to linger.”
Public-domain text, read in full here on John Shaqi.
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