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
As already remarked the formation we have described is that of almost
the whole Red Sea, but south of Suakin it loses the regularity that
is so noticeable northwards. The area marked on the map (p. 126)
as “Suakin Archipelago” consists of innumerable small reefs,
shoals and islets, the water between being of very irregular
depth, three hundred fathoms being found close alongside surface
reefs. Opposite Trinkitat the water shoals gradually, only 30 to
40 fathoms being found as far as 45 miles from land. The shore
itself is extremely low and sandstone hills are absent. The area
marked Shubuk, south of Suakin, shewn on the map enclosed by a
thin semicircular line on the north and east sides and by the land
on the west and south, has a very remarkable structure. An area
of 100 square miles is enclosed by a regular and unbroken reef,
indicated by the above curved line, the space within being a most
intricate maze of reefs with comparatively deep canal-like passages
between them. In the south are broader passages and some islets of
elevated coral. The bounding reef is extremely regular and, on its
eastern side, unbroken. It consists of a steep slope and precipice
of growing coral up to near the surface, when the slope becomes very
gradual and forms a nearly smooth surface of stunted corals with grey
_Xenia_. This extends to among the breakers, above which is a band of
gravel formed of broken and wave-rounded pieces of coral. Within is
sand, and the coral capped sandbanks of the labyrinth. Landwards the
ground is for miles so low and so much broken into by salt lagoons
and marshes that a definite coast-line can scarcely be said to exist.
This is the remains of an old delta of the Khor Baraka, a river which
rises in the Abyssinian highlands, but which nowadays never reaches
the sea. Its floods come down on to the maritime plain at Tokar,
where, spreading over a considerable area, they render possible
the growth of cotton and other crops in the fine soil they leave
soaked with water. Tokar is thus the one fruitful spot of any size
on the whole Red Sea coast, but its character of fertile oasis is
but short-lived. When the crops are gathered even the dry cotton
stalks must be removed lest they should collect the sand, which,
every day of the summer, is carried over them by burning gales,
and so would convert the fertile ground into barren sandhills.
As it is, at any rate at present, impossible to predict these floods
the seed must be sown after each, even though it frequently happens
that another flood comes down and carries it all away. The seed must
then be patiently re-sown, and that left by the last flood will grow
and bear. In the old days, before man was there to make any use of
it, the Baraka formed a regular delta, subject to yearly floods,
a miniature Egypt. The growth of coral in this neighbourhood would
then be impossible, the shifting sand, muddy and freshened water
rendering its life impossible.
Public-domain text, read in full here on John Shaqi.
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