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
Everything connected with the village is of the most primitive
description, and until a very short time ago few of the inhabitants
had been beyond the limits of their own fields. The advent of
the railway caused no little commotion and stir in the oasis,
and awakened trading instincts which had lain dormant since Roman
times. Many of the villagers now travel to and fro between Kharga
and the Nile Valley, and the Omda took an early opportunity of
obtaining leave of absence from his onerous duties, and proceeded
to Alexandria for a course of sea-baths!
Outside the village, with the exception of the antiquities, to which
we shall call attention in a separate chapter, there is little of
general interest beyond the wells and gardens, among which there
are many picturesque spots. At Bir Ain el Gôs, a few kilometres
to the north, a primitive form of corn-mill may be seen working,
the grinding-stones being driven by the water of the well by means
of an undershot wheel.
It may be mentioned here that with very few, if any, exceptions
the different streams which collectively make up the water-supply
of the oasis find their way to the surface through artificially
constructed passages. The great majority of these are bores of
ancient construction, though a few have been sunk with modern plant
during the last fifty years. The ancient wells are known as Aiyûn
(sing. Ain), the modern as Abiyâr (sing. Bir); for example,
Ain el Ghazâl, Bir Mansûra. In cases where a modern bore has
been specially sunk to replace an ancient well, the two words are
used in conjunction; for instance, Bir Ain el Gôs. The position of
each well is nearly always conspicuously marked by a thick clump of
acacias, from which (more especially in the isolated settlements in
the northern part of the depression) the main irrigating channel
generally runs in a southerly direction, the cultivated lands
being of triangular form, with the apex at or near the source of
the water, and raised little, if at all, above the general level
of the surrounding plain. By this disposition the fields present
the least possible front to the north, from which side comes the
bulk of the sand which is such a curse to these outlying settlements.
Public-domain text, read in full here on John Shaqi.
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