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
When eventually we reached our destination, some 15 to 20 metres
beyond the last man-hole, it was only to find that the tunnel just
stopped. There was no more water emerging from the rock at the
end than I had seen entering at a dozen small fissures along the
course we had traversed; there was no vertical excavation downwards;
there were no traces of inscriptions; nothing, in fact. After all
our trouble, we had drawn a blank. Although I positively dreaded
the long crawl back, the very fact that every step took us towards
the fresh air made me feel comparatively cheerful. After making my
examination of the end of the tunnel, however, I found the space was
insufficient to allow of my turning round, so that I was compelled
to proceed backwards for some distance before I found room in which
to turn. I must confess to never having experienced such a feeling
of relief as when we eventually arrived at the bottom of the open
shaft, and were able to fill our lungs with copious draughts of the
air descending from above. We could see the tiny pin-hole of light
far above us, and when sufficiently rested we swung the rope as
a signal to be wound up. Although I got back to the surface none
the worse for my adventure, with the exception of skin bruises,
I would not recommend anyone to attempt the exploration of other
similar tunnels unless there were open shafts on either side to
insure some circulation of air.
It is now quite certain that the aqueducts derived their water
from the numerous small fissures traversed, so that the yield
of any single tunnel must have depended to a great extent on its
total length. The general formation of the country determined the
general direction of the tunnels, which, in order to keep within
reasonable distance of the surface, had to follow the valleys. The
latter, without exception in this district, run in a north and
south direction, having formed at one time drainage-lines from the
high plateau to the north. Many of the short branch tunnels are,
however, driven along east and west fissures, though these could
not be followed to any great distance, owing to the high ridges
separating the valleys. It is also quite certain that the work of
excavation was eventually stopped by the ever-increasing labour
involved in the construction of the vertical shafts, the depth of
which necessarily increased at a rapid rate as the surface of the
ground rose when nearing the actual escarpment. For instance, in the
space of only 230 metres, between the ninth and the first shafts,
the depth of the man-holes increases from 40 to 54 metres, and to
the north of this the increase would have been still more rapid,
until the amount of vertical excavation would have become altogether
disproportionate to the horizontal distance gained by the aqueduct.
CHAPTER XIII
BORING METHODS: ANCIENT AND MODERN
Public-domain text, read in full here on John Shaqi.
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