The Prehistoric World; Or, Vanished RacesAllen, Emory Adams
History
The Prehistoric World; Or, Vanished Races
Allen, Emory Adams
Archaeology; Indians; Prehistoric peoples
Mention has been made of the Eskimo traits still to be observed
among the tribes of California. Prof. Putnam thinks that this
fact can best be explained on the supposition that these tribes
came in contact with primitive Eskimo people.66 Dr. Rink, from
investigation of the language and traditions of the different
Eskimo tribes, thinks they are of American origin, and must once
have lived much farther south.67 He says, “The Eskimos appear to
have been the last wave of an aboriginal American race, which has
spread over the continent from more genial regions— following
principally the rivers and water-courses, and continually
yielding to the pressure of the tribes behind them until they
have at last peopled the sea-coasts.”68 Mr. Dall, in his
explorations of the Aleutian Islands, comes to the same
conclusion as Dr. Rink. He says his own conclusions are, “that
the Eskimos were once inhabitants of the interior of North
America—have much the same distribution as the walrus, namely, as
far south as New Jersey.”69
All this tends to prove that the Paleolithic people of New Jersey
were ancestors of the Eskimos. This becomes highly probable when
we pursue the subject a little farther. Dr. Abbott has shown,
from the similarity of implements, position in which found, and
so forth, that the Paleolithic people continued to occupy the
country down to comparatively recent times, when Indian relics
took their place.70 This is such an important point that we must
give his reasons more in detail. Remember that Dr. Abbott speaks
from the experience gained by gathering over twenty thousand
specimens of stone implements, and paying especial attention to
the position in which they were found. The surface soil of that
section of New Jersey, where he made his explorations, was formed
by the slow decomposition of vegetable and forest growth. In this
layer he found great numbers of undoubted Indian implements. The
number, however, rapidly decreases the deeper we go in this
stratum. This would show that the Indians were late arrivals.
Below this surface soil is a stratum of sand, overlying the
gravelly beds below and passing into the surface soil just
mentioned. In this layer were found great numbers of implements
inferior to the Indian types found on the surface, but superior
to the Paleolithic specimens described. They are not only
inferior in finish to the Indian specimens, but are of different
material. They are always formed of argillite. It was further
noticed that the number of these rapidly decreased in the layer
of surface soil, and are but rarely found on the surface.
Public-domain text, read in full here on John Shaqi.
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