The Atlantic Monthly, Volume 12, No. 69, July, 1863: A Magazine of Literature, Art, and PoliticsVarious
General
The Atlantic Monthly, Volume 12, No. 69, July, 1863: A Magazine of Literature, Art, and Politics
Various
American periodicals
Within the Periods there is a still more limited kind of geological
division, founded upon the special character of local deposits. These I
would call geological Formations, indicating concrete local deposits,
having no cosmic character, but circumscribed within comparatively narrow
areas, as distinguished from the other terms, Ages, Epochs, Periods, which
have a more universal meaning, and are, as it were, cosmopolitan in their
application. Let me illustrate my meaning by some formations of the
present time. The accumulations along the coast of Florida are composed
chiefly of coral sand, mixed of course with the remains of the animals
belonging to that locality; those along the coast of the Southern States
consist principally of loam, which the rivers bring down from their swamps
and low, muddy grounds; those upon the shores of the Middle States are
made up of clay from the disintegration of the eastern slopes of the
Alleghanies; while those farther north, along our own coast, are mostly
formed of sand from the New-England granites. Such deposits are the local
work of one period, containing the organic remains belonging to the time
and place. From the geological point of view, I would call them
Formations; from the naturalist's point of view, I would call them
Zooelogical Provinces.
Of course, in urging the application of these names, I do not intend to
assume any dictatorship in the matter of geological nomenclature. But I do
feel very strongly the confusion arising from an indiscriminate use of
terms, and that, whatever names be selected as most appropriate or
descriptive for these divisions, geologists should agree to use them in
the same sense.
There is one other geological term, bequeathed to us by a great authority,
and which cannot be changed for the better: I mean that of Geological
Horizon, applied by Humboldt to the whole extent of any one geological
division,--as, for instance, the Silurian horizon, including the whole
extent of the Silurian epoch. It indicates one level in time, as the
horizon which limits our view indicates the farthest extension of the
plain on which we stand in space.
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