An Egyptian oasis : $b An account of the oasis of Kharga in the Libyan desert, with special reference to its history, physical geography, and water-supplyBeadnell, H. J. L. (Hugh John Llewellyn)
History
An Egyptian oasis : $b An account of the oasis of Kharga in the Libyan desert, with special reference to its history, physical geography, and water-supply
Although flint implements have never yet been detected _in situ_
in the lacustrine deposits, I have collected a considerable
number from the area originally occupied by the lake. Some of
these were found lying on the denuded surfaces of the lake beds,
in positions which lead me to suppose that they have weathered out
from the deposits. They are decidedly Neolithic in workmanship and
character, and were, in my opinion, used by people inhabiting the
depression at the time of, and probably prior to, the existence of
the lake. A number of examples are shown in one of the accompanying
plates; the figure in the bottom left-hand corner is, however,
that of a palæolith, a typical example of those which occur on the
borders of the plateau, and on or near the eastern escarpments. In
the right-hand bottom corner is figured an object of very common
occurrence in the oasis—a sandstone hand-grinder, probably of
Roman age. With the exception of these two the specimens illustrated
are all implements from the site of the lake. Flint implements
were evidently in use in Kharga at a very late period, as large
numbers of worked flints, mostly in the form of flakes or tools of
very poor finish, occur near many of the old sanded-up wells. A
considerable amount of detailed work will have to be undertaken
before the different flints of the oasis can be satisfactorily
arranged in chronological order.
From what period did the lake date, and to what cause did it owe its
origin, are questions which cannot, I fear, be definitely answered
as yet. While it is quite reasonable to consider, in the absence
of any decisive evidence to the contrary, that the lake originated
in early prehistoric or Pleistocene times—that it dates possibly
from the time of the formation of the tufas of the Nile Valley and
oasis-escarpment, when the climate was certainly much moister than
at the present day—we must not forget the possibility that it
was formed by artificial means during one or other of the Egyptian
dynasties between 3000 and 1000 B.C.
Public-domain text, read in full here on John Shaqi.
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