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
I now propose to review briefly the question of the age of our
so-called paleolithic implements, the questions of the _grade_ of
a given feature of culture and of the _age_ or chronologic place
of that culture being very properly treated separately, as they
depend for their support upon distinct classes of evidence. During
the past summer, 1892, certain important items of new evidence have
been discovered bearing upon the question of the occurrence or
non-occurrence of rudely flaked stones or of any artificial objects
whatsoever in the normal gravels of the Delaware Valley, and it
therefore becomes necessary to examine somewhat critically such of the
published evidence as seems to be seriously affected by these recent
observations.
It may be stated in beginning that no one disputes the glacial age of
the Trenton gravels. The question to be discussed is simply this,--is
the evidence satisfactory that works of art have been found in these
gravels? Nothing else need be asked or answered. I do not take up
this subject because I love controversy; disputation is really most
distasteful to me. It happens that under the Bureau of Ethnology of the
Smithsonian Institution I have been assigned to the work of making a
survey of the archeology of the Atlantic coast region in which large
areas, especially in states south of Mason and Dixon's line, remained
almost untouched by investigators, and two years have been consumed
mainly in these southern areas. But there are questions that refuse
to be confined to definite geographic limits, and evidence secured in
one section is sometimes found to bear so directly and forcibly upon
problems pertaining primarily to other sections that the student of
these problems must perforce become a free lance, and unhesitatingly
enter any province promising results of value, howsoever fully occupied
it may be by other investigators. One of the most interesting and
important questions growing out of the study of American archeology
has, as we have seen, arisen in the Delaware Valley, and the turn taken
by some of my work in the south and west is such that I cannot pass
this question by without consideration. The necessity of taking up
the subject of glacial man became more and more apparent as the years
passed on, and people continued to say to me, "You must go to Trenton;
we are not satisfied with the present status of the question there; the
evidence arrayed in favor of the theory of a paleolithic gravel man
needs critical examination."
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