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 construction during recent years of extensive irrigation works
in the Nile Valley has made it possible to largely augment the
water-supply of the Bahr Yusef to the Fayûm. High level canals are
being cut in various parts of the district and already large areas of
desert covered by these lacustrine deposits have been brought under
cultivation, notably to the north of Tamia and in the neighbourhood
of Qasr Qurûn. The approximate area covered with lacustrine deposits
can be seen on the map and with a sufficiency of water probably the
greater part of this area could be utilized, though the exact value
of the soil compared with Nile deposit remains to be determined.
SECTION II.—THE BIRKET EL QURUN.
The lowest part of the depression, lying immediately to the north-west
of the cultivation, is occupied by a sheet of water of considerable
size, known as the Birket el Qurûn.[7] The lake, which has a length of
40 kilometres, and a maximum breadth under ten, covers at the present
time an area of about 225 square kilometres. Sir Hanbury Brown obtained
no sounding exceeding 5 metres in crossing the lake to Dimê, but
according to the fishermen the depth increases towards the south-west.
Its long axis lies nearly east and west, and while on the north it is
entirely[8] bordered by desert, along a large part of the south side
the cultivated land approaches its shore, although even here a large
area actually bordering the lake is waste salty land as yet unfit for
cultivation. As already mentioned, with the exception of the Gharaq
basin, the lake receives the whole drainage from the cultivated lands.
The Birket el Qurûn is the existing remnant of the ancient prehistoric
lake which covered a large part of the floor of the Fayûm depression,
and which in historic times was converted into an artificially
controlled sheet of water—the celebrated Moeris—by Amenemhat I
and his successors in the XII Dynasty.
Lake Moeris, being used as a regulator of excessively high and low
Nile floods,[9] was of the greatest importance in connection with
the irrigation of the Nile Valley. In more recent times, apparently
under the Persians or Ptolemies according to Flinders Petrie,[10]
Lake Moeris ceased to perform its function of regulator; since that
time all water, except that required for irrigation of the reclaimed
land, being carefully excluded, the surface of the lake has continually
and gradually sunk to its modern dimensions.[11]
Public-domain text, read in full here on John Shaqi.
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