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
The bay is on three sides completely enclosed by cliffs and its
floor is thickly covered by a luxurious growth of wild scrub—chiefly
tamarisk and ghardag; numerous isolated palm trees occur, especially in
the neighbourhood of the water which exists at several points. There
are three particularly good springs,[25] the positions of which are
shown on the accompanying maps. According to Colonel Western’s
survey the water emerges at about + 20 metres. In 1899 the water of
the northern spring was found to have a temperature of 26°C. On our
last visit we found an artificially constructed pool of two metres
diameter and a depth of 30 centimetres; on the west side of this
were two springs, marked by the motion of the grey sand rising and
falling in the vents, down which a stick could be easily pushed to
a depth of two metres. The output of these springs together amounted
to six litres a minute; the water was quite clear and although soft
and rather ferruginous not by any means unpalatable (see analyses
below). The pool lies on an open bare sandy spot and is surrounded by
scattered bushes, none of which however are within fifteen metres;
a sand dune lies 150 metres to the south-west, with bushes and
seven or eight young palms. The southerly spring has an output of
21 litres a minute, and its water does not differ essentially from
that of the northern spring. Rising at the foot of a palm tree it
forms pools on either side; thence it flows a distance of 20 metres
into an artificially constructed shallow basin 2 to 3 metres across,
from which it runs away down the slope and disappears after five or
six metres. The east spring, which is situated on the east side of
the dunes bounding the mouth of the bay, consists of a small hole cut
out in soft sand. The water seemed good, although analysis shows the
salts content to be high; this spring does not run, but if emptied
the hole soon refills. The remains of old buildings occur near the
well, in the shape of loose roughly squared limestone blocks, broken
pottery, and remains of old walls; the latter are nearly level with
the ground and very thickly and solidly built.
To the south of the promontory lies the so-called Little Rayan. Here
there is a good deal of scrub, and water can be obtained on the lowest
ground at a few metres depth, although there do not appear to be any
surface springs.
[Sidenote: Geology of Wadi Rayan in broad outline.]
Public-domain text, read in full here on John Shaqi.
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