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
[Illustration: PLATE I.
NORTH SIDE OF THE BIRKET EL QURUN, LOOKING WEST.]
SURVEY DEPARTMENT,
EGYPT.
* * * * *
THE TOPOGRAPHY AND GEOLOGY
OF THE
FAYUM PROVINCE
OF EGYPT
BY
H. J. L. BEADNELL, F.G.S., F.R.G.S.
[Decoration]
CAIRO
NATIONAL PRINTING DEPARTMENT
1905.
CONTENTS.
* * * * *
INTRODUCTION.
PAGES.
Surveying operations. Soil survey. History of discovery of
Fayûm vertebrate fauna 9
PART I.—TOPOGRAPHY AND STRUCTURAL GEOLOGY.
SECTION I.—CULTIVATED LAND—
Area. Composition and character of alluvial soil. Connection
with Nile Valley. Bahr Yusef and canal system. Ravines.
Alluvial deposits of Lake Moeris and prehistoric lake.
Increase of cultivated lands 11
SECTION II.—THE BIRKET EL QURUN—
Site, depth and dimensions. Remnant of Lake Moeris. Continual
shrinkage of lake. Deposition of sand in lake at present day.
Salinity of lake. Possible underground outlets. Currents 12
SECTION III.—THE SURROUNDING DESERT REGION—
Area and limits of Libyan Desert described. Rocks forming the
area. Importance of dip. Chief causes of origin of Fayûm 14
SECTION IV.—WADI RAYAN AND NEIGHBOURHOOD—
Colonel Western’s survey. Sir William Willcocks’ report.
Borings. Details of proposed reservoir. Schweinfurth’s
estimate of salt content. Willcocks’ “Assuan Reservoir and
Lake Moeris.” Detailed geological examination not yet
undertaken. Traverse from Nile Valley through Wadi Muêla and
Rayan to Gharaq. Warshat el Melh and springs of Wadi Muêla.
Der el Galamûn. Pass from Muêla to Rayan. Sand accumulations.
Wadi Korif. Springs of Wadi Rayan. Analyses and output of
water. Geological succession in Wadi Rayan. General geology of
floor and bounding walls. Ridge separating Rayan and Gharaq.
Apparent absence of Nile deposit and freshwater shells in Wadi
Rayan. Question of leakage through ridge. Permeability of Rayan
if used as a reservoir. Salinity of water 16
SECTION V.—CENTRAL AREA OF THE REGION—
Area and features. Dip-slope of surface. Drainage basins of
central plain. Pools formed by rainfall. Tamarisk growth. The
eastern area covered by alluvium. The bounding plateau to the
north. Ghart el Khanashat dunes 24
SECTION VI.—THE RIDGE SEPARATING THE NILE VALLEY AND FAYUM—
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