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
-------------------------+---------------+--------------+-------------
| NORTH SPRING.| SOUTH SPRING.| EAST SPRING.
-------------------------+---------------+--------------+-------------
Matter In Solution | 398·8 | 350·8 | 811·6
| | |
Chlorine calculated as | | |
Sodium Chloride | 278·4 | 238·2 | 585·5
| | |
Sulphur Trioxide | | |
calculated as | | |
Sodium Sulphate | 62·9 | 53·9 | 126·2
The above figures are parts per 100,000 parts of water.
Although the above analyses prove the water to be of a very poor
quality for drinking purposes, compared with many of the wells
and springs of the oases, the water, which is quite clear, seemed
good. Except for its softness and somewhat ferruginous taste, it
is quite palatable, and on my last visit we used no other for five
days. The south spring was found to yield 21 litres and the north 6
litres per minute. The water of the third spring does not run.]
[Illustration: PLATE IV.
WESTERN EXTREMITY OF THE BIRKET EL QURUN.]
PART II.
=TECTONICS.=
* * * * *
SECTION VIII.—FAULTING AND FOLDING.
[Sidenote: The Fayûm Depression formed by subaerial Erosion.]
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account