An Egyptian oasis : $b An account of the oasis of Kharga in the Libyan desert, with special reference to its history, physical geography, and water-supplyBeadnell, H. J. L. (Hugh John Llewellyn)
History
An Egyptian oasis : $b An account of the oasis of Kharga in the Libyan desert, with special reference to its history, physical geography, and water-supply
Solitary barchans, being well-defined isolated masses, lend
themselves to observation better than the large and continuous
belts of sand. They occur of all sizes, from little baby crescents,
a metre or two across, to enormous masses 30 or 40 metres high and
200 to 300 metres in breadth. In all cases, except when their steady
march southwards has been temporarily interrupted by southerly
winds, the southern face, flanked by the horns of the crescent,
is a straight slope of from 30 to 33 degrees, its inclination is,
in fact, the angle of rest of loose dry sand, and it is formed
of the sand which is continually blown up the opposite slope and
dropped over the crest.
In a moderate breeze the whole barchan progresses steadily in a
southerly direction without loss or gain of sand; in stronger winds,
while still continuing its course, the dune may at the same time
be either losing or gaining in actual bulk. The rate at which the
barchans travel varies with their size. The larger the dune the
greater the amount of material to be moved, so that, as a general
rule, small barchans progress much more rapidly than large ones. The
actual rate may vary from 10 to 20 metres per annum, the average
being about 17. For instance, the big isolated dune on the road
between Headquarters and Kharga village moved 11 metres southwards
between December 8, 1907, and December 8, 1908, while during the same
period a small dune in the Bellaida district travelled 21 metres in
the same direction. The dimensions of these two dunes is as follows:
+------------------------------------+-------------+----------+
| | Kharga Road | Bellaida |
| | Dune. | Dune. |
+------------------------------------+-------------+----------+
| | Metres. | Metres. |
| Vertical height of centre of crest | 17 | 10·5 |
| Maximum breadth (east and west) | 259 | 160 |
| Maximum length (north and south) | 230 | 70 |
+------------------------------------+-------------+----------+
These are merely instances from dunes which I have had under
observation for a number of months, full details of which I hope
shortly to publish.
Public-domain text, read in full here on John Shaqi.
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