Desert and water gardens of the Red Sea : $b Being an account of the natives and the shore formations of the coastCrossland, Cyril
Science
Desert and water gardens of the Red Sea : $b Being an account of the natives and the shore formations of the coast
Crossland, Cyril
Coral reefs and islands; Red Sea; Sudan -- Social life and customs
Obviously this canal-like inlet is not the mouth of a river, past
or present, for present rivers there are none, and no river, flowing
over a wide plain, through loose and heterogeneous materials, could
cut out such a channel, but would end in a wide shallow estuary or
delta, if it formed a definite mouth at all.
The new harbour of Port Sudan is much wider both in the entrance
and within, but the origin of this deep landlocked basin is equally
puzzling.
The forms of all the harbours of the coast can be reduced to one
plan more or less easily, that of a cross with arms parallel and
at right angles to the coast-line, and are in fact formed by two
cracks in the earth’s surface nearly at right angles. The former
arm is generally the largest, in Port Sudan it is two miles long, the
other arm, which connects this with the sea and forms the shallower
branch harbour, being much the shorter. The same applies to for
instance Wiai, Fîjab, Salak Seghir and Ankêfail Kebir, whereas in
the case of the narrower harbours, like Suakin, Arûs, Shinab and
its neighbours, the arm at right angles to the sea is the longest,
and the plan of the inlet is more like the conventional cross.
[Illustration: Fig. 90. Two of the canal-like “Khor” which
run into the coral plain. Soundings in fathoms, note comparatively
great depth of the water
The arrow in Khor Shinab indicates the point at which the material
of the cliff changes from coral to gravel.]
In Wiai, Fîjab, Salak Seghir and other harbours most of the land
between the inner arm and the sea, corresponding to the East Town
in Port Sudan, has been cut down
[Illustration: Fig. 91]
and converted into reef, upon which strips of sand have accumulated
to form islands in places. In all three harbours currents flowing in
and out have buried the south end of this reef, next the entrance
passage, in a steep sandbank (the point is marked by an arrow on
the plans). As the water is too deep for convenient anchorage of
small vessels, the _sambûks_ run their noses on to these sandbanks,
a couple of sailors walk ashore with the anchor, and they are moored
for the night, as the prevailing wind is from the north.
Salak Seghir has a long narrow winding entrance, like a deep still
river between reefs. Having successfully but fearfully navigated
this in my launch, I found that my sailors’ design was to
run her on to the sandbank, _sambûk_ fashion. I declined this,
for my copper sheathing’s sake, and was all unprepared for the
fact that the passage there is about as wide as my launch is long
and that the inner branch is shallow and full of humps of coral,
giving me a choice of evils which I do not intend to make again. The
sand lying on the reef between the inner harbour and the sea has
become consolidated into sandstone in a narrow parallel-sided band,
perfectly level and almost as regular as an artificial breakwater. A
short length of such a formation would be striking, but this extends
to nearly two miles.
Public-domain text, read in full here on John Shaqi.
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