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
Above the Qasr el Sagha series, and well marked off from them both
lithologically and palæontologically, is found a great thickness of
variegated sands, sandstones, clays and marls, the “Fluvio-marine
Series” (Jebel el Qatrani beds), divided near the summit by
one or more thick intercalated lava sheets, the latter forming a
convenient junction line. This series of variegated beds is of Upper
Eocene—Lower Oligocene age.
No Miocene strata have been recognized within the area, but further
north, as at Mogara, Lower Miocene deposits occur;[34] and it is
probable that there is a continuous series of lithologically similar
beds from the summit of the Fayûm escarpments (Lower Oligocene)
to the Mogara Miocene.
The Pliocene is probably represented by the great terraces of
gravel—raised beaches—which are such a marked feature in the
geology of the district. Fossiliferous Pliocene deposits have also
been recorded from the south part of the area by Schweinfurth.[35]
Pleistocene and Recent are abundantly represented by lacustrine clays,
both ancient and modern, alluvial land and blown sand, the formation
of which deposits is continuing at the present time.
The following table will show the sequence of strata and the
classification adopted in the present memoir:—
TABLE SHOWING SUCCESSION AND CLASSIFICATION OF STRATA IN THE FAYUM.
-----------+---------+--------+-----------+---------------------------
| | |Approximate|
| | | average |
| | | thickness |
| | | in metres,|
| | | north part|
| | | of Fayum. |
| | +-----------|
| | | | Alluvial soil, clays,
| | | | sands, etc.
RECENT | | | |
AND | | | | Blown sand.
PLEISTOCENE| | | |
| | | | Lacustrine clays,
| | | | extending to about 23
| | | | metres above sea-level.
-----------+---------+--------+-----------+---------------------------
| | | | Gravel Terraces (?
| | | | Pleistocene).
| | | |
(MIDDLE?) | | | | Shell-borings on rock
PLIOCENE | | | | surfaces.
| | | |
| | | 50 | Fossiliferous deposits of
| | | | Sidmant.
-----------+---------+--------+-----------+---------------------------
| | | |_Fluvio-marine Series
| | | |(Jebel el Qatrani beds)_.
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