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
Long before the dawn of the Columbian era, therefore, the Amerind
peoples had become, through the influences indicated, a world-race by
themselves, existing in various stages of the same general culture,
and with a rising and a declining of tribes and stocks directed by
environment and circumstances. The great stocks surviving at the
beginning of the Columbian era may be approximately traced by their
languages, in layers, from Panama northward, about as they expanded
mainly eastward of the Sierra Nevada in response to the gradual relief
from the pressure of the cold. The Yucatec tribes had held the region
south of the Tehuantepec isthmus, and owing to this slight barrier,
and perhaps to another barrier of a strait through the land about
on the line of the proposed Nicaragua canal, had developed somewhat
differently from tribes to the north, and may also have preserved
more of their original character. Thence stretching north far into
the United States was the great composite Shoshone, or Uto-Aztecan
family, in all its variations, with what appears to be an “island” of
Athapascans or Boreal men preserved in its midst by glacial conditions
lingering in the high regions near the Mexico-United States line;
then follows the Siouan; then the widespread Algonquian stock; next
the Athapascan; and finally the Eskimauan, which had always been held
against the edge of the glaciers by the back pressure of the southern
stocks, and being most remote was less affected by filtration from
the development centre, and thus remains to-day a more differentiated
stock than any other.[3] The western arm of these stocks was generally
farther north than the eastern because the climate was and is milder
in the west, the trend of the ice front being now, and apparently
always having been, N.W. to S.E. Distribution of skill in pottery
follows about the same lines, “petering” out with stocks farthest
from the Yucatec centre. The Algonquins crowded the Athapascans off
to the N.W., and together they crowded the Eskimo to the limits of
human subsistence. In California many stocks found refuge in a climate
kept comparatively mild by the ocean currents, where they secured
subsistence on fish, and went no farther south. Along the Gulf coast
were other tribes resting somewhat aside from the great continental ebb
and flow, while in Florida and in the islands of the Caribbean region
there was sufficient separation to produce a slight differentiation
from the surging continental stocks. Remnants of other stocks were
scattered here and there through the regions below the glaciated
area. Mingled with all these developments there were probably certain
traits and “tinges” derived from earlier ancestry, and these, with the
similarity of development of all races under like conditions prevailing
wherever human beings can live, fully account for resemblances to
other-world tribes and peoples that have caused so much speculation.
Public-domain text, read in full here on John Shaqi.
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