Principles of Geology: or, The Modern Changes of the Earth and its Inhabitants Considered as Illustrative of GeologyLyell, Charles, Sir
Science
Principles of Geology: or, The Modern Changes of the Earth and its Inhabitants Considered as Illustrative of Geology
Lyell, Charles, Sir
Geology
We learn from Mr. Hodgson's account of the mammalia of Nepal, that the
tiger is sometimes found at the very edge of perpetual snow in the
Himalaya;[134] and Pennant mentions that it is found among the snows of
Mount Ararat in Armenia. The jaguar, also, has been seen in America,
wandering from Mexico, as far north as Kentucky, lat. 37° N.,[135] and
even as far as 42° S. in South America,--a latitude which corresponds to
that of the Pyrenees in the northern hemisphere.[136] The range of the
puma is still wider, for it roams from the equator to the Straits of
Magellan, being often seen at Port Famine, in lat. 53° 38' S.
A new species of panther (_Felis irbis_), covered with long hair, has
been discovered in Siberia, evidently inhabiting, like the tiger, a
region north of the Celestial Mountains, which are in lat. 42°.[137]
The two-horned African rhinoceros occurs without the tropics at the Cape
of Good Hope, in lat. 34° 29' S., where it is accompanied by the
elephant, hippopotamus, and hyæna. Here the migration of all these
species towards the south is arrested by the ocean; but if the continent
had been prolonged still farther, and the land had been of moderate
elevation, it is very probable that they might have extended their
range to a greater distance from the tropics.
Now, if the Indian tiger can range in our own times to the southern
borders of Siberia, or skirt the snows of the Himalaya, and if the puma
can reach the fifty-third degree of latitude in South America, we may
easily understand how large species of the same _genera_ may once have
inhabited our temperate climates. The mammoth (_E. primigenius_),
already alluded to, as occurring fossil in England, was decidedly
different from the two existing species of elephants, one of which is
limited to Asia, south of the 31° of N. lat., the other to Africa, where
it extends, as before stated, as far south as the Cape of Good Hope. The
bones of the great fossil species are very widely spread over Europe and
North America; but are nowhere in such profusion as in Siberia,
particularly near the shores of the Frozen Ocean. Are we, then, to
conclude that this animal preferred a polar climate? If so, it may well
be asked, by what food was it sustained, and why does it not still
survive near the arctic circle?[138]
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