The Journal of Geology, January-February 1893: A Semi-Quarterly Magazine of Geology and Related SciencesVarious
Science
The Journal of Geology, January-February 1893: A Semi-Quarterly Magazine of Geology and Related Sciences
Various
Geology -- Periodicals
That the art remains of the Trenton region are essentially a unit,
having no natural separation into time, culture or stock groups,
is easily susceptible of demonstration. I have already presented
strong reasons for concluding that all the finds upon the Trenton
sites are from the surface or from recent deposits, and that all may
reasonably be assigned to the Indian. A find has recently been made
which furnishes full and decisive evidence upon this point. At Point
Pleasant, on the Delaware, some twenty-five miles above Trenton, there
are outcrops of argillite, and here have been discovered recently the
shop sites upon which this stone was worked. There are two features
of these shops to which the closest attention must be given. The
first is that they are manifestly modern; they are situated on the
present flood plain of the Delaware, and but a few feet above average
water level, the glacial terrace here being some forty or fifty feet
in height. These shops, therefore, represent the most modern phases
of aboriginal industry, and may have been occupied at the coming of
William Penn. The second point is that every type of flaked argillite
found in the Trenton region, associated with the gravels or otherwise,
is found on this site. It was to a certain extent a quarry site, for
the great masses of argillite brought down by the floods were here
broken up and removed from the river banks or bed. It was a shop site,
for here the articles, mainly blades, were roughed out, and it was
also a dwelling place--a village site--where all the specialized forms
of flaked stones made from the blades were prepared for use. Here are
found great numbers of the rude failures, duplicating every feature
of the mysterious "paleolith" with which our museums are stocked,
and exhibiting the same masterly quitting at just the point "where
no further shaping was possible."[7] Here we see the same boldly
manipulated "cutting edge," the "flat bottom" and "high peak," and the
same mysteriously weathered and disintegrated surfaces, so skillfully
made, by a nice balancing of accidents,[8] to tell the story of
chronologic sequence in deposition.
[7] Abbott, C. C. Smithsonian Report, 1875, p. 248.
[8] Ibid. Primitive Industry, p. 487.
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