The Prehistoric World; Or, Vanished RacesAllen, Emory Adams
History
The Prehistoric World; Or, Vanished Races
Allen, Emory Adams
Archaeology; Indians; Prehistoric peoples
But in spite of these difficulties, attempts have been made from
time to time to determine the absolute chronology of these ages.
The results, however, can only be considered as approximations of
the truth. We will call attention to some of these calculations.
Their value to us consists in showing us the methods by which
this problem has been attacked, and not in the results obtained.
M. Morlot, of Switzerland, has sought to determine this question
by a study of the delta of the Tinière, which is a small river
flowing into the lake of Geneva. Like all mountain streams, it
brings down considerable quantities of sediment, with which it
has formed a conical shaped delta. Cuttings for a railroad
exposed a fine section of this cone, and showed that at three
different times layers of vegetable soil, which must once have
been its old surface were found.
The lowest surface was some twenty feet beneath the present
surface, and here were found relics of the Stone Age. The second
layer was at the depth of ten feet, and contained relics of the
Bronze Age. Finally the first buried layer, three feet beneath
the present surface, was found to contain relics of the Roman
Age. Obtaining from other data the time that has elapsed since
the deposits of the Roman layer, he readily calculates the age of
the Stone and Bronze layers. By this means he obtains for the
Bronze Age an antiquity of between three and four thousand years,
and for the Neolithic Age from five to seven thousand years.17 M.
Morlot does not claim for his calculation more than approximate
accuracy.18 But if we were to allow it a greater accuracy than
its author claims, it would still only show us that from a period
of from five to seven thousand years ago, tribes of stone using
folks lived in Switzerland. It tells us nothing as to their first
appearance, or the total length of this age.19
Other calculations of a similar nature have been made. The Lake
of Bienne, in Switzerland, has been gradually silting up along
its margins from time immemorial. About seven hundred and fifty
years ago there was an abbey built at one place on the then
existing shore of the lake. Since that time the gain of land has
been about twelve hundred feet. A considerable distance further
up the valley are found the remains of a lake settlement of the
Stone Age. If the gain of land has been uniform, it has not been
far from seven thousand years since the lake washed round the
ancient settlement. Of course the land may have gained faster at
one time than at another, but from the general configuration of
the valley it is considered that its gain was regular.20
Public-domain text, read in full here on John Shaqi.
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