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
One of the longest cross-country traverses I myself have undertaken
in the Libyan Desert was from Farafra Oasis to Assiut. The only
road between that oasis and the Nile Valley strikes the latter
near El Qusîya, midway between the towns Manfalut and Derut, so
that travellers who wish to make Assiut have an additional day’s
march southwards alongside the margin of the cultivated lands. On
gaining the summit of the pass above Bir Murr, on the east side
of the Farafra depression, I abandoned the road and set a course
direct for Assiut, steering and plotting my route by compass and
plane-table, the distance being reckoned by measuring-wheel. The
most satisfactory method of procedure on desert traverses is to lay
out a line, representing the correct bearing of the destination,
along the centre of the longer axis of the plane-table, and then
to steer to any well-marked object lying on either side, but within
reasonable distance, of the proper course. At every station the exact
position reached is plotted, and steps are taken, when selecting
the next point on which to march, to converge towards the correct
course marked down the centre of the table.
On this particular traverse I was unaccompanied by Europeans or
Bedawin, my camel drivers being fellahin from the Nile Valley. The
surface proved excellent going, and the Abu Mohariq belt of dunes,
190 kilometres from Qasr Farafra, was crossed without trouble. Eight
days after leaving Farafra village we struck the escarpment of
the Nile Valley, having covered nearly 300 kilometres, and found
we were marching on a point only very little to one side of the
town of Assiut. From this traverse it was possible to calculate
the longitude of Farafra with fair accuracy.
The normal rate of travelling of camels carrying ordinary loads
weighing from three to four hundred-weight is 4 kilometres, or
about 2½ miles, an hour, ten hours being the usual day’s march
of caravans when accompanied by Europeans. The native caravans,
carrying dates and other heavy merchandise, usually traverse
the plateau in three days and nights, doing stages of 60 to 70
kilometres at a stretch. By travelling very light with trotting
camels I have, on more than one occasion, crossed from the oasis
to the valley in between thirty and thirty-five hours, doing from
180 to 190 kilometres in two stages of about twelve hours each,
with one stop only of nine or ten hours.
CHAPTER IV
TOPOGRAPHY AND GEOLOGY
Dimensions of the Oasis-Depression — Jebel Têr, Jebel Tarif,
and other Hills within the Depression — Aspect of the Oasis from
the surrounding Escarpments — Geological Sequence — Nature and
Thickness of the Strata — Geological History of the Oasis —
Formation of the Depression — Difference of Level of Strata on
either side of the Depression — The Great Longitudinal Flexure
— Height of the Floor compared with Sea-Level — Altitudes.
Public-domain text, read in full here on John Shaqi.
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