Proceedings of the expedition to explore the northern coast of Africa, from Tripoly eastward : $b in MDCCCXXI. and MDCCCXXII., comprehending an account of the Greater Syrtis and Cyrenaica; and of the ancient cities composing the pentapolisBeechey, Frederick William
History
Proceedings of the expedition to explore the northern coast of Africa, from Tripoly eastward : $b in MDCCCXXI. and MDCCCXXII., comprehending an account of the Greater Syrtis and Cyrenaica; and of the ancient cities composing the pentapolis
Beechey, Frederick William
Sidra, Gulf of (Libya); Tripoli (Libya) -- Antiquities; Tripoli (Libya) -- Discovery and exploration
It is difficult to say on what authorities the narrow inlet was
originally introduced which terminates the gulf in the charts above
mentioned; unless, indeed, the terms which have been used by ancient
geographers, in describing this part of the Greater Syrtis, may be
supposed to have occasioned the idea. The castle of Automala is
mentioned by Strabo as situated in the _innermost recess_ of the
gulf[2]. And Pliny speaks of the coast inhabited by the Lotophagi
(which he places in the Greater Syrtis) as being equally in the
_innermost_ part of the bay[3]. It may be possible that these terms
have induced the more recent geographers to consider the gulf
as terminating in an inlet, and to hazard, on their authority,
the introduction of that which is now in question in the absence
of any accurate survey. If such meaning can be supposed to have
been extracted from the term used by Strabo, his authority might
certainly have been safely relied upon by those who employed it
on this occasion without any reproach to their caution; since this
geographer himself visited the coast in a vessel, and may therefore
be supposed to have seen what he described. However this may be,
we can positively assert that no inlet whatever exists in the Gulf
of Syrtis; and that the direction of the coast at the bottom of the
gulf is, as nearly as possible, due east and west for a whole day’s
journey together; turning afterwards to the northward so slightly,
that this difference is scarcely perceptible to the eye. A large
tract of quick sand is also laid down by many in this part of the
Gulf of Syrtis; but we have traversed the sand and the sand-hills
which are found here, on horseback, in almost every direction,
and may safely affirm that they afford as good a footing as any
dry sand or sand heaps can be supposed to present. If any other
authority may be acceptable in proof of the extreme dryness of the
sand in this neighbourhood, we have only to cite that of Doctor
Della Cella to put everything like scepticism on this point at
rest. “Woe be to us,” exclaims this gentleman, (in describing
the sandy tract here alluded to) “if a sirocco, or southerly wind,
had unhappily overtaken us in this place, the whole army would have
been buried beneath the sands which the action of the winds here
raised up in waves no less formidable than those of the sea!”
Now if anything like moisture had really existed in the formidable
particles which caused the Doctor such alarm, he might have looked
in defiance at every point of the compass, without anticipating,
with so much well-described horror, the fatal consequences which
would have resulted to himself and the whole army, had the wind
been unfortunately to the southward.
Public-domain text, read in full here on John Shaqi.
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