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
Apaches and Navajos are usually said to have _come down_ from their kin
in the North, but it is equally possible that they _remained behind_
in the high mountains while their kin pushed on.[398] The table-lands
of Mexico, being high and temperate, formed a final refuge for many
tribes, some of whom had profited by contact with the centre of
development, and these roamed the plateau, one branch finally settling
around the lake of Mexico, and there planting again the seeds of the
lowland culture. Many tribes were early crowded into the California
coast region, because the lowland climate there remained comparatively
mild, and the supply of fish, seals, etc. was so great that they were
not compelled to till the soil for subsistence (if indeed they were
possessed of sufficient knowledge, or if the land were in condition
to produce), as was the case farther south, where the population
was denser and natural supplies insufficient. But the region was so
inhospitable that only fragments of these tribes survived. They did not
multiply.
[Illustration: PROBABLE ASPECT OF ALASKA SUMMER LANDSCAPE SOME 600
YEARS AGO
Harriman Alaska Expedition, 1899. Photographed by the author
]
The reason the Eastern continents produced many and diverse peoples is
that the glacial period temperate zone, or warm zone, extended through
many degrees of _longitude_, offering extensive areas of settlement to
the races in that hemisphere, where they remained more or less isolated
and independent, to advance in their own way and along their own lines;
that is, on the Eastern continents there was ample _latitudinal_ land
space, while on the Western there was a very limited latitudinal land
space that retained a salubrious climate. This was the cause of North
American race homogeneity.
Public-domain text, read in full here on John Shaqi.
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