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
Commencing work at Sêla, on the eastern side of the depression, the
survey was carried northwards along the east side of the cultivated
lands and thence through the northern desert, up to the summit
of the depression. After mapping westwards as far as the isolated
hill-mass of Gar el Gehannem the work was temporarily suspended until,
in the spring, the narrow defile of Wadi Muêla, and the Wadi Rayan,
forming the southern part of the Fayûm depression, were provisionally
examined.
In January 1901, samples of soil and water from the cultivated lands
were collected as an experimental soil-survey, and the results have
been published.[1]
During the winter’s work of 1902-03 a traverse was carried from Gar
el Gehannem in a south-west direction through a hitherto unexplored
part of the depression. On reaching a point midway between Cairo
and the oasis of Baharia a connection was made eastwards to Wadi
Rayan. In the winter of 1903-04 further exploration was carried out
in the neighbourhood of Gar el Gehannem.
It will be convenient here to briefly relate the history of the
discovery of the remarkable series of new and extinct animal forms, the
recovery of which from the Fayûm deposits has created such widespread
interest in the zoological world. When Schweinfurth crossed the region
in 1879 he obtained fossil bones, which were examined and determined
by Dames to be the remains of cetacea of the genus _Zeuglodon_,
from certain beds of the escarpment west of Qasr el Sagha; these,
it is believed, were the earliest vertebrate remains obtained from
the Fayûm. During the early part of the survey of the district,
remains of fish and crocodiles were frequently found in one of the
beds of the Middle Eocene, probably on the same horizon as that
from which Schweinfurth had collected. Fragments of bone were also
commonly met with on a much higher horizon (_i.e._, near the base
of the Fluvio-marine series) but nothing of particular interest
was obtained, as no detailed search could be made at that time. In
April 1901, during the survey of the western end of the Birket el
Qurûn, some of the localities found to be bone-bearing in 1898 were
re-visited in company with Dr. C. W. Andrews, who was in Egypt at the
time and had accompanied the survey in order to obtain specimens of
jackals, hares, etc., for the British Museum, in connection with the
forthcoming work on Egyptian mammals. In one of these Dr. Andrews
picked up several vertebrae which turned out to belong to a new
species of _Pterosphenus_.
Public-domain text, read in full here on John Shaqi.
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