The principal villages of Baharia are four in number, all situated
near together in the north part of the oasis in N. lat. 28° 21′
to 28° 22′. They are separated into two groups by a large hill
(Jebel Mandisha), El Qasr and Bawitti lying to the west, and Mandisha
and Zubbo to the east. The Government officials reside at Bawitti
and El Qasr. According to the last census,[31] the population of the
oasis in 1897 was 6,081 divided among the four villages as follows:—
El Qasr 1.712
Bawitti 1.713
Mandisha 1.798
Zubbo 858[32]
The males slightly outnumber the opposite sex.
The villages are small uninteresting collections of mud hovels,
surrounded by gardens, palm-groves, and cultivated lands. Besides
the cultivated tracts existing close around the villages, there
are others at points more or less distant from them, tilled by men
from the villages. Such are seen, for instance, west of Zubbo;
at Ain Bayum, a spring with a small cultivated area, among the
sand-dunes 4½ kilometres north-east of Zubbo, where a clump of
date-palms forms a conspicuous landmark; Ain Sini and Ain Murun,
7 kilometres north-east of El Qasr; also some small tracts west of,
and a large area south-west of, Bawitti. Ain Auena, El Ayun, and other
points marked on Ascherson’s map, are probably within this last
area. Taking the whole cultivated land, inclusive of palm-groves,
at 11 sq. kilometres, the area per individual of population works
out to about 0·43 feddans; this figure is somewhat lower than
Kharga (0·56 feddan) and considerably less than that of Dakhla
(1·49). While Kharga exports practically nothing, Baharia does a
considerable export trade with the Nile Valley, principally in dates,
although not on so large a scale as Dakhla.
In and near the villages springs are extremely numerous; the water
is met with at shallow depths, and does not require, as in Kharga and
Dakhla, deep-bored wells. It is led from its sources along underground
aqueducts, which date from the Roman occupation; a description of
these will be found in the chapter on antiquities (p. 73-80). No
attempt was made by the survey to map or number the wells and springs
within the vicinity of the villages; they are mostly concealed in
the palm-groves and gardens. The water is slightly ferruginous,
and frequently warm, bubbles of carbon dioxide rising with it. At
Bawitti, the largest spring is cold, but one close by it is warm,
although none approach the high temperature of the Dakhla wells. One
of the principal sources of water in Mandisha, is a well, situated
near the cemetery, 7 metres deep and timbered with palm trunks;
the temperature of the water is 26° C. (air 12° C.), and when
freshly drawn it is turbid with bubbles of carbon dioxide.[33]
Public-domain text, read in full here on John Shaqi.
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