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
Of the history of the oases during the succeeding seven or eight
centuries no records are available, but, judging from the writings
of Arabian geographers, between the eleventh and the fifteenth
centuries, it is evident that they gradually became depopulated, and
were regarded as of little importance. El Sherîf el Edrissi, writing
about the middle of the sixth century of the Hegîra, refers to the
oases (Al Vahat) as places formerly containing streams of water,
with lands on which trees were still found growing, and with ruined,
uninhabited towns. He adds that the goats and sheep had become quite
wild, and were trapped by hunters like other wild animals. It is
not improbable, however, that this author was referring to some of
the smaller oases-depressions, such as Kurkur, or perhaps to some
of the more outlying parts of Kharga or Dakhla. It seems extremely
unlikely, as Hoskins remarks, that the Great Oasis as a whole had
become entirely uninhabited.
Still later the emir and historian Ismail Abulfida, about the
beginning of the fourteenth century, speaks of the oases as abounding
with palms and running water, and describes them as situated like
islands, in the middle of the desert, three days’ journey from the
Said (Upper Egypt). Jacutus describes the positions of three oases,
and refers to the first of them as being well cultivated, containing
streams and hot springs, palms and cultivated lands. The inhabitants,
he adds, are in a wretched state. Several other writers allude
to the Egyptian oases, but their information is seldom, if ever,
first hand, and the descriptions are in general so vague that we
are left in doubt as to which particular oasis their remarks refer.
The more modern records, commencing with those of Poncet at the
end of the seventeenth century, have already been referred to in
a previous chapter.
CHAPTER VIII
THE EXTINCT LAKES OF THE OASIS
Character and Extension of Lacustrine Deposits — Modern Erosion
by Wind-borne Sand — The Lakes geologically of Recent Age
— Discovery of Pottery and Bones of Domesticated Animals —
Area occupied by the Lakes — Maximum Level of their Waters —
Lacustrine Strata at Gorn el Gennâh — Relation to the Ancient
Monuments — Altitudes of Archæological Sites — Age of the Lakes
and their Persistence into Historic Times — Flint Implements
— Origin of the Lakes — Their possible connection with the
Artesian Waters — Lacustrine Deposits form the Cultivated Lands
of Modern Times.
Public-domain text, read in full here on John Shaqi.
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