Geology -- Egypt; Nile River; Water-supply -- Egypt
The water-supply of the oasis is derived from an underground bed of
sandstone, 55 metres thick, underlying a dense impervious red clay 45
metres in thickness; the upper part of the latter is conspicuous
throughout the oasis, underlying the alluvium and forming the base of
the surrounding escarpments in many localities. Below the water-bearing
sandstone lies a black clay, never yet penetrated by the boring rods; it
is probable that other water-tables exist below and such would be
invaluable for the irrigation of those parts of the oasis where the
present supply is unsatisfactory. There seem to be no natural springs
extant at the present day, the whole of the water-supply being through
boreholes, both ancient and modern. The old wells, known as _ain_,
_aiyûn_, appear to be mostly of early Egyptian and Roman construction,
and number over 400; exactly similar wells have been sunk by boring
plant during the last few decades and are called _bîr_, _biyâr_; there
are over 160 of these; all are true artesian wells. At the present day
the method in vogue is as follows:--a two metre square timbered shaft is
sunk by hand to the base of the red clay and within this is built up a
watertight wooden pipe, 35 cm. in diameter, made of ‘sunt’ (a species of
thorny acacia), the surrounding space being packed with clay. Sinking is
continued in the sandstone with the boring machine until a satisfactory
flow of water is obtained. Many of the older wells in the oasis have
become choked up, and although some have been successfully cleaned out
by the inhabitants, but the process is costly and laborious and
frequently fails. The work is done by divers, a small but hardy class
only found in Dakhla and Farafra.
Public-domain text, read in full here on John Shaqi.
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