The Prehistoric World; Or, Vanished RacesAllen, Emory Adams
History
The Prehistoric World; Or, Vanished Races
Allen, Emory Adams
Archaeology; Indians; Prehistoric peoples
Accordingly, when Professor Whitney states as the result of many
years spent in the investigation of the Tertiary formation of
California, that he finds evidence of the existence of man in the
Pliocene Age, it is not strange that one part of the scientific
world listens incredulously to his statements, and are at once
ready to explain away the facts on which he relies. He may, of
course, be mistaken, for it is human to err, but his proofs are
sufficiently strong to convince some of the best scholars in
America. We can do no more than to lay the facts before the
reader and let him judge for himself.
We have seen what a genial climate prevailed in Europe during the
Tertiary Age. This must also have been true of California. A rich
and varied vegetation decked the land. The great trees of
California of our day then flourished in Greenland, Iceland, and
Western Europe. The cypress of the Southern States was then
growing in Alaska and other high northern latitudes. The climate
probably passed from a tropical one, in early Tertiary times, to
a milder or temperate one in Pliocene times. Amongst the animals
inhabiting America were three species of camels. Rhinoceroses,
mastodons, and elephants trooped over the land. Tigers and other
carnivore prowled in the forests. Herds of horse-like animals,
one scarcely distinguishable from our common horse, grazed in the
valleys, along with several species of deer. From the presence of
the old drainage beds, we know that majestic rivers rolled their
watery burden through the land. Such a country might well afford
a home for man if he were present.
To understand fully the course of events which now took place we
must venture on geological ground. The great Pacific Ocean, lying
to the west of America, is constantly exerting a lateral
pressure, which during Tertiary times showed its effect in the
uplifting of the great mountain ranges of the western coast.2
During late Tertiary times, as a counterpart to the upward
movement, a great subsidence commenced in the Pacific region.3
Doubtless many islands, some think an entire continent even,
disappeared beneath the waves. The completion of the various
mountain ranges left the coast firm and unyielding; hence, as it
could not bend before the fiery flood forced upward from below by
the downward motion just mentioned, it broke, and the torrent of
molten rock leaped out as a lava flow. In consequence of this,
near the close of Pliocene times, the surface of California and
Oregon, especially the north of California, became buried under
the lava and ashes of the most desolating volcanic outbreak that
the earth has ever known.
Public-domain text, read in full here on John Shaqi.
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