The topography and geology of the Fayum province of EgyptBeadnell, H. J. L. (Hugh John Llewellyn)
Science
The topography and geology of the Fayum province of Egypt
Beadnell, H. J. L. (Hugh John Llewellyn)
Geology -- Egypt
We are here on the summit of the divide between Wadi Muêla and Wadi
Rayan, the height of the floor being about + 105 metres; to the north
stretches a gradually widening bay descending to the lowest ground
of the Rayan depression. Immense accumulations of sand almost block
the defile and stretch away to the east, and the hitherto well-marked
cliff on that side bends back and is lost to view. On the other side
however, the bounding wall gradually emerges from the dunes, getting
more distinct as it is followed northwards until it becomes quite
clear of the sand. The first glimpse of this cliff is seen a couple of
kilometres west of the pass in an outcropping headland, the next point
visible being some five kilometres further west. Between these portions
of the cliff are one or two outliers, surrounded by quantities of blown
sand. A depression known as Wadi Korif is reported to lie to the west,
and much scrub and some water is said to exist there; such a wadi is
marked on Schweinfurth’s map but apparently has not been examined.
Continuing in a N.N.W. direction high rather steep dunes occur
on either flank, running N.N.W. and S.S.E. Between the dunes is a
fairly hard undulating sand-flat affording an easy route; further
on a narrow defile between the dunes leads down to the centre of
the depression. The main areas occupied by blown sand are shown in
the accompanying maps. The most interesting part of the depression
is the bay lying to the south of the narrow well-marked promontory
jutting out from the southern plateau, a huge pointer, as it were,
in the direction of Gharaq; this is the Cape Rayan of Schweinfurth.
[Sidenote: Springs in Wadi Rayan.]
Public-domain text, read in full here on John Shaqi.
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