The topography and geology of the Fayum province of Egypt — John Shaqi
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
In the lowest spots the saline frequently consists of soft wet sludge;
its area is about half a square kilometre but the depth of the deposit
is unknown. In the middle of the scrub-covered area to the north lies
Ain Warshat el Melh, a pool of water, fairly fresh and drinkable,
although ferruginous, measuring 10 by 5 metres in size and from 2
to 2½ metres deep. The water evidently rises from a spring on the
west side, round which are fifty square metres of green rushes, with
some larger bushes. The ground around and above is very saliferous;
between the spring and the ruins to the north the ground is sandy,
with many bushes and much scrub. This ground extends two kilometres
to the west, whence it gradually passes up into great masses of drift
sand; an occasional small outcrop of the top of the plateau above the
sand is all that serves to locate the position of the buried cliff. On
the east side the sandy ground with scrub extends about a kilometre,
beyond which the plain gradually rises for another kilometre to the
base of the cliff beyond, which is fairly steep and well-marked,
though with an entire absence of indentations of any kind.
[Sidenote: Der el Galamûn.]
Close to the north end of the valley, and about 33 kilometres from
El Gayat, lie the ruins known as Der el Galamûn bil Muêla. At
the time of our visit a new square stone building was in course of
erection and five or six persons were inhabiting the place. There are
several small palms scattered about to the south of the monastery and
an excellent running spring of clear water five hundred paces to the
south-west. A new well is being sunk within the premises. To the north
of the monastery the eastern cliff takes a marked trend to the west
for some three kilometres, whence it resumes a northerly direction,
always maintaining its character of a steep well-marked escarpment
rising some 100 metres above the floor of the wadi. At the corner
of the cliffs the lowest bed exposed is a white limestone; this is
overlain by gypseous clays passing up into sandy beds, the latter
being surmounted by the white limestone capping the escarpment.
[Sidenote: Wadi Rayan.]
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account