The romance of natural history, second seriesGosse, Philip Henry
History
The romance of natural history, second series
Gosse, Philip Henry
Natural history
Hugh Miller has an interesting observation concerning the actual date of
geologic phenomena in North America, compared with that of their
counterparts in the Old World. He says, "The much greater remoteness of
the mastodontic period in Europe than in America is a circumstance
worthy of notice, as it is one of many facts that seem to indicate a
general transposition of at least the later geologic ages on the
opposite sides of the Atlantic. Groups of corresponding character on the
eastern and western shores of this great ocean were not contemporaneous
in time. It has been repeatedly remarked that the existing plants and
trees of the United States, with not a few of its fishes and reptiles,
bear in their forms and constructions the marks of a much greater
antiquity than those of Europe. The geologist who set himself to
discover similar types on the eastern side of the Atlantic, would have
to seek for them among the deposits of the later tertiaries. North
America seems to be still passing through its later tertiary ages; and
it appears to be a consequence of this curious transposition, that while
in Europe the mastodontic period is removed by two great geologic eras,
from the present time, it is removed from it in America by only
one."[11]
Professor Agassiz has expressed opinions of the same character, adducing
the present existence in America of several forms of animals, which are
known in this hemisphere only in a fossil state.[12]
I cannot refrain from adding the following combination of fact and
speculation, from the pen of an accomplished traveller in Mexico. It
opens up a new train of ideas:--
"Some time before our visit, a number of workmen were employed on the
neighbouring estate of Chapingo, to excavate a canal over that part of
the plain from which the waters have gradually retired during the last
three centuries. At four feet below the surface, they reached an ancient
causeway, of the existence of which there was of course not the most
remote suspicion. The cedar piles, by which the sides were supported,
were still sound at heart. Three feet below the edge of this ancient
work, in what may have been the very ditch, they struck upon the entire
skeleton of a Mastodon, embedded in the blue clay. Many of the most
valuable bones were lost by the careless manner in which they were
extricated; others were ground to powder on their conveyance to the
capital, but sufficient remained to prove that the animal had been of
great size. My informant measured the diameter [_qu._ circumference?]
of the tusk, and found it to be eighteen inches.
Public-domain text, read in full here on John Shaqi.
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