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
The actual width of the plateau varies from 120 kilometres between
Abu Sighawâl and the scarp above Waled Hallaf, to 200 kilometres
between Beris and Esna. The maximum elevation above sea-level
is about 550 metres on the latitude of Esna, and on the whole
the plateau has a fairly general slope to the north. As already
mentioned, several distinct types of country, depending on the nature
of the rocks constituting the surface strata, are met with. Smooth,
hard, level plains, formed of a superficial layer of weathered
limestone covered by a brown veneer of insoluble flint and cherty
fragments, alternate with bare rugged rock desert of hummocky
limestone. The sombre level or gently undulating flint-covered
plains, frequently spoken of as ‘serir’ by the Arabs, have
ideal surfaces for travelling; the light-coloured hummocky country,
often called ‘kharafish,’ is in its most developed form made
up of innumerable elongated hillocks, every portion of the exposed
rock-surfaces being deeply scored; the furrows are separated by
upstanding edges, often so sharp and knife-like as to be capable
of injuring the feet of man and beast. The hillocks are separated
by deep troughs half buried in drift-sand, all lying parallel,
in the direction of the prevailing winds, so that progress in a
latitudinal direction through this type of desert is a slow and
tedious undertaking. Both types of country are equally desolate and
barren, scrub of any description being of the rarest occurrence,
except after local thunderstorms. Another type of country, to which
we have already briefly alluded, is the curious desert-surface called
El Botîkh (the water-melons), which results from the weathering
of certain bands of the Lower Eocene formation containing numbers
of large globular concretions; these, it may be mentioned, often
lie so thickly strewn on the surface as to actually obstruct the
passing caravan.
Kharga is connected with the oasis of Dakhla to the west by two
roads, the lower and more southerly, known as the Derb el Ghubbâri,
being the one most frequently used. This road, by taking a wide
sweep to the south, avoids the intervening plateau altogether,
so that the fatiguing ascent and descent are avoided. After
leaving Kharga village the route leads past a group of wells,
known as Ain Khenâfish, distant some 6 kilometres; thence it lies
over wide-stretching plains of sandstone, leading up to the more
broken country formed by the foot-hills of the towering plateau,
which is always plainly visible on the north side of the road. The
distance to Tenîda, the most easterly of the Dakhla villages,
is 143 kilometres by the Derb el Ghubbâri.
Public-domain text, read in full here on John Shaqi.
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