The geography and geology of south-eastern EgyptBall, John
Science
The geography and geology of south-eastern Egypt
Ball, John
Geology -- Egypt; Physical geography -- Egypt
The =Springs of Abu Saafa= are situated in the Wadi Hodein, about two
kilometres below the point of influx of Wadi Gihab, at an altitude of
310 metres above sea-level. The Wadi Hodein is here narrow, and shut
in by very high steep sandstone scarps. There are four springs, all
issuing from the northern scarp at intervals of about sixty metres
along the wadi, and all about three metres above the wadi floor,
trickling into pools about a metre in diameter close by. The most
westerly of the four springs is a mere trickle; the next yields a
rather greater flow, from a carved niche in the rock, with a Greek
cornice; the third is the one most used, having the greatest flow
of the four, while the easternmost is almost stagnant and has yellow
incrustations near it. The rate of flow, even from the largest spring,
is very slow, probably not more than ten litres per minute, and
the overflow from the pools is only a tiny stream a few centimetres
wide which soon loses itself in the sand of the wadi floor; but the
pools are large enough for a dozen or more camels to drink from, and
soon fill up again when emptied. The water is of excellent quality,
very clear, and the supply never fails. Near the springs there are
five or six small date palms, and the wadi hereabouts has many other
trees. After rain, this part of Wadi Hodein at times becomes a stream;
this was the case in October 1907, for I found numerous pools in the
wadi floor, and scum and froth showing that an impetuous stream about
half a metre deep had flowed down the wadi only a few days prior to my
visit. Just below Abu Saafa Springs, Wadi Hodein receives the short
=Wadi Maghal= from the north-west; this wadi, which is walled in by
high sandstone plateaux, contains water holes about three kilometres
from Wadi Hodein; but these are less important than the springs of
Abu Saafa, and are, moreover, off the main road.
Public-domain text, read in full here on John Shaqi.
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