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
The word ‘oasis’ is old Egyptian, as also is the Arabic
‘wah,’ the latter word being also found in Coptic, and signifying
an inhabited place; nevertheless, the word ‘wah’ was never used
by the ancient Egyptians to designate the oases. These they called
‘otu,’ which means a place where bodies are embalmed. ‘Otu’
has its origin in the Theban myth, according to which Seth, the
murderer of Osiris, was pursued by Horus to Koptos, where he was
captured and thrown into a dungeon. His corpse was afterwards
found by his friends, and taken to the oases for burial.[1] The
inscriptions on the temple of Hibis in Kharga refer to the oases
under the comprehensive name ‘Set-ament,’ the ‘Western
Lands.’
About the same time Dr. Schweinfurth, whose services to Egypt in
so many branches of science stand pre-eminent, published important
contributions on some of the archæological remains. Two or three
years later Brugsch Bey brought out an account of the antiquities
of the oasis, with translations of a number of the inscriptions on
the temples of Nadûra and Hibis. The antiquities will be briefly
referred to in my account of the history of the oasis under the
Persians and the Romans, and for fuller details the reader is
referred to the publications of Cailliaud, Hoskins, Schweinfurth,
Brugsch, and some still later writers.
In 1893-94 Captain H. G. Lyons, R.E., in the course of a military
patrol, undertaken in order to ascertain the measures necessary
to protect the inhabitants of the oasis from possible Dervish
raids, made valuable geological observations on the Eocene and
Cretaceous systems, especially in relation to the connection of
folding and water-supply. These he discussed in a paper read before
the Geological Society of London in 1894, and it was mainly due to
the interest it aroused, and to his initiative in pointing out to
the Egyptian authorities the importance of having a comprehensive
examination of the country carried out, that the Geological Survey
of Egypt was established in 1896.
The detailed survey of the Libyan Desert was taken up in October,
1897, and completed in June of the following year, the four
oases being mapped on the scale of 1 to 50,000 by plane-table
triangulation, checked and adjusted by numerous astronomical
observations. Direct measurements by measuring-wheel were also
employed to a considerable extent. Baharia Oasis was the first to be
taken in hand, Mr. Leonard Gorringe and I taking the western side,
and my colleagues, Messrs. Ball and Vuta, the eastern. This plan of
splitting up an oasis-depression between two surveying parties was
not, however, found satisfactory, and on the completion of Baharia
it was decided that Ball should take up the oasis of Kharga, while
Farafra and Dakhla fell to my lot. The results of this survey are
published in the Memoirs of the Geological Survey of Egypt.
Public-domain text, read in full here on John Shaqi.
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