The Highlands of EthiopiaHarris, William Cornwallis, Sir
History
The Highlands of Ethiopia
Harris, William Cornwallis, Sir
Ethiopia -- Description and travel
Dame Nature must indeed have been in a most afflicting throe to have
given birth to a progeny so monstrous; and there being no locality to
which the most vivid fancy could assign aught that ever bore the name of
wealth or human population, little doubt can exist that the sea must
have been repelled far from its former boundaries. The oviform figure
of the bowl, hemmed in on three sides by volcanic mountains, and on the
fourth by sheets of lava, would at the first glance indicate the site of
an extensive crater, whose cone having fallen into a subterranean abyss,
had given rise to the singular appearance witnessed. But it is a far
more probable hypothesis that the Bahr Assal, now a dead sea, formed at
some very remote period a continuation of the Gulf of Tajura, and was
separated from Goobut el Kharab by a stream of lava six miles in
breadth, subsequently upheaved by subterranean action, and now forming a
barrier, which, from its point of greatest elevation, where the traces
of many craters still exist, gradually slopes eastward towards the deep
waters of the bay, and westward into the basin of the Salt Lake. Whilst
no soundings are found in the estuary of Tajura, Goobut el Kharab gives
one hundred and fifteen fathoms, or six hundred and ninety feet; and
premising the depression of the lake to have been formerly correspondent
therewith, one hundred and twenty feet may be assumed as its present
depth. To this it has been reduced by the great annual evaporation that
must take place--an evaporation decreasing every year as the salt
solution becomes more intensely concentrated, and evinced by the saline
incrustation on the surface no less than by a horizontal efflorescence,
in strata, at a considerable height on the face of the circumjacent
rocks.
In the lapse of years, should the present order of things continue
undisturbed from below, the water win probably disappear altogether,
leaving a field of rock salt, which, when covered in by the debris
washed down from the adjacent mountains, will form an extensive depot
for the supply of Danakil generations yet unborn; and the shocks of
earthquakes being still occasionally felt in the neighbourhood, it seems
not improbable--to carry the speculation still further--that Goobut el
Kharab, divided only by a narrow channel from the Bay of Tajura, will,
under subterranean influence, be, in due process of time, converted into
a salt lake, in no material respect dissimilar from the Bahr Assal--
another worthy type of the Valley of the Shadow of Death.
Volume One, Chapter XV.
DISMAL NIGHT-MARCH ALONG THE INHOSPITABLE SHORES OF THE GREAT SALT LAKE.
Public-domain text, read in full here on John Shaqi.
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