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 — John Shaqi
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
For the first few kilometres the main road from Abu Sighawâl runs
very straight over a level plain, on which fossil sea-urchins are
so abundant as to attract the attention of the most casual observer;
it then ascends a low escarpment, the Nagab el Jellab. The somewhat
rough limestone country beyond is known as the Mishâbit, and then El
Botîkh, with its countless millions of spherical chert concretions,
is crossed. Beyond El Botîkh the road passes an isolated limestone
hill called El Mograbi, where tradition has it that a Mograbi
Arab from the west and his stolen oasis bride were overtaken and
decapitated by the Kharga people. A little farther to the east there
is a bifurcation, but the branches soon rejoin, and after passing El
Masaâd the plain is fairly level, though covered with very angular
blocks of crystalline limestone and cherty concretions. Farther on
are the rocks of El Buraig, where large quantities of broken pottery
indicate the site of one of the many water-stations maintained
by the Romans along this road. Garat el Melh is so called from
the occurrence of salt in the limestones of this locality. A few
kilometres to the east of Garat el Melh the road passes El Suâga,
an artificial heap of stones to which every self-respecting Bedawi
is careful to contribute; and a couple of hours beyond, a fairly
conspicuous limestone hill, called Garat Radwan, is reached.
Shortly after passing Garat Radwan the most prominent landmarks
met with on this road, in the form of two solitary crescent-shape
sand-dunes, loom into sight; these are called El Ghart by the Arabs
and are distant 55 kilometres from Abu Sighawâl. They form part
of a belt of single isolated dunes which crosses this part of the
desert in a N.N.W. and S.S.E. direction. The same line of dunes
is passed by the railway at kilometre No. 100, and I have observed
its continuation still farther north on the Sohag road, at a point
45 kilometres from the Refûf pass. These dunes mark the entrance
to an area of very rough hummocky crystalline limestone known as
El Zizagat, through which the track is not easily followed. On
emerging from El Zizagat the road bears slightly to the north, and
is here only a few kilometres south of El Tundaba. At this point it
bifurcates, the northern branch proceeding direct to Waled Hallaf
near Girga, the southern continuing over the easy level plains of El
Ishab to the rocks of El Baglûli, and thence past those of Dilail
el Kelb to the twin hillocks of Dubîya. Beyond El Dubîya the road
crosses the shallow drainage-line of Rod el Ghanam, near the head
of the Wadi Samhûd, down which it passes, and thence over the Nile
Valley plains past El Hamera and Hagar Hawara to Karnak and Farshut.
Public-domain text, read in full here on John Shaqi.
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