Scientific American, Vol. XXXVII.—No. 2. [New Series.], July 14, 1877: A Weekly Journal of Practical Information, Art, Science, Mechanics, Chemistry, and Manufactures — John Shaqi
Scientific American, Vol. XXXVII.—No. 2. [New Series.], July 14, 1877: A Weekly Journal of Practical Information, Art, Science, Mechanics, Chemistry, and ManufacturesVarious
Science
Scientific American, Vol. XXXVII.—No. 2. [New Series.], July 14, 1877: A Weekly Journal of Practical Information, Art, Science, Mechanics, Chemistry, and Manufactures
Various
Science -- Periodicals; Technology -- Periodicals
In this Mr. King has unquestionably rendered good service to the
science he has done so much to extend and honor in the field; while
the illustrations from American geology which he brings to bear on the
subject are as likely as his sturdy opinions to attract attention.
Yet we are inclined to think that in some things he has allowed his
enthusiasm to run away with him. The stolid self-confidence of
extreme Uniformitarians has tempted him to exaggerate the periodic
accelerations of geologic and biologic movement, and to overstate
their effects quite as much as others have underestimated them;
and when he charges the followers of Lyell with intellectual
near-sightedness and a lack of "the very mechanism of imagination,"
they may possibly be able to retort not unjustifiably that he has
mistaken the natural foreshortening of the geological vista due to
distance for actual brevity; and that his belief in the abruptness and
suddenness of the great changes which the earth's strata record, may
be due to his own lack of sustained imaginative power for grasping and
interpreting all the evidences of the enormous time really involved.
But this is a question not of imaginative capacity but of logical
deduction from observed facts; and however abrupt the beginning of
some of the great geologic movements may have been, their subsequent
progress cannot in all cases have been so rapid as to allow of their
being called catastrophic in any ordinary acceptation of the term.
Take, for example, the alleged catastrophe which marked the close of
the mesozoic age in the West. Of this movement Mr. King remarks: "In
a quasi-uniformitarian way, 20,000 or 30,000 feet of sediment had
accumulated in the Pacific and 14,000 in the [American] mediterranean
sea; when these regions, which, during the reception of sediment,
had been areas of subsidence, suddenly upheaved, the doming up of the
middle of the continent quite obliterating the mediterranean sea and
uniting the two land masses into one. The catastrophe which removed
this sea resulted in the folding up of mountain ranges 20,000 and
40,000 feet in height, thereby essentially changing the whole climate
of the continent."
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account