The North-Americans of yesterday : $b a comparative study of North-American Indian life, customs, and products, on the theory of the ethnic unity of the raceDellenbaugh, Frederick Samuel
History
The North-Americans of yesterday : $b a comparative study of North-American Indian life, customs, and products, on the theory of the ethnic unity of the race
Dellenbaugh, Frederick Samuel
Indians of Mexico; Indians of North America
The cause of the glacial period has been much discussed. It seems to
have been largely due to changes in land levels,[394] and to other
causes not now understood. The people inhabiting the world before it
may have been originally much alike in kind and colour with local
variations, and the isolation produced by glacial conditions modified
this colour and increased the variations, those finally left in hot
lands becoming darker, medium temperatures producing brown, still
cooler the reds and yellows, and the forests of Europe evolving a shade
or shadow people, shrinking from the strong sun; the so-called white
race. The glacial epoch is often spoken of as if the whole world were
frozen solid, whereas in North America, from the Ohio and the Columbia
to the Isthmus, the climate was doubtless about relatively the same
as it is now from Davis Strait to the Potomac and from Yakutat Bay to
northern California. The ice extended down about to the Ohio River
in the East and on lowlands not below the Columbia in the West. The
Western mountain tops must have been completely glaciated and all
elevated regions were cold, the conditions prevailing resembling those
now found in Southern Alaska. The Sierra Nevadas, receiving the warm,
moist airs from the Pacific, must have been far more heavily glaciated
than the Rockies, which received less moisture in consequence. The ice
period is estimated to have endured from ten to twenty thousand years,
with an interval of recession in it and subsequent advance. The people
were driven southward, and those most favourably situated developed the
most. The people most favourably situated were all _who were already
in_, or could fight their way to, the temperate lowlands of southern
Mexico and Central America, which were rendered somewhat more extensive
by the recession of the sea, caused by the withdrawal of the immense
quantities of water that were heaped up in ice thousands of feet in
thickness.[395] This has been estimated to have lowered the waters of
the ocean by from 600 to 1000 feet.[396] The lands thus laid bare were
climatically inviting and probably were soon covered with vegetation.
In South America the people were crowded northward, or held there by
the cold coming from the south. It would be in the northern portions,
particularly the lowlands, that we ought to find evidence of the
highest development, especially on the side receiving warm currents,
and there is where we do find it. We apparently have then a northern
and a southern limit to the ancient inhabitants of this hemisphere,
within which climatic conditions during the period of great cold, and
for some time thereafter, were most favourable to human development.
This limit in the Northern continent is latitude 23 and in the Southern
also 23. Within these lines the great precolumbian development took
place, and the heart of this development on the Northern continent
seems to have rested between the Isthmus of Tehuantepec and the present
Public-domain text, read in full here on John Shaqi.
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