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
[Footnote 8: (Leo Africanus in Ramusio, p. 72.)—With respect to
the former extension of Tripoly to the northward, here mentioned
by the African geographer, the observation is certainly in some
degree correct, and consistent with the present appearance of other
parts of the coast of Northern Africa; but we must at the same time
observe that the town could scarcely have projected any farther
to the northward than the sites of the French and Spanish forts;
for beyond these we get into five and eight fathoms water.]
[Footnote 9: We must, however, confess, that we cannot altogether
understand, why the loss of the ground in the immediate neighbourhood
of Tripoly, said by Leo Africanus to have been flooded in his days,
should have necessarily occasioned to the inhabitants of the town so
great a scarcity of grain as that mentioned by this geographer. For
the high grounds immediately beyond the parts which were overflowed,
must at all times, we should conceive, from their rocky foundation,
have been placed above the level of the sea at its greatest height,
and might therefore have been cultivated as we find them to be
at present; and the Gharian mountains, as well as the country of
Tagiura, both of which are still very productive, are mentioned
by Leo as places highly cultivated at the period of the overflow
alluded to.
We may remark on this subject—that the coincidence of the former
with the present state of the last-mentioned places, appears to be
the more worthy of notice, from the circumstance of our finding the
actual produce of other districts, both in Tunis and Tripoly, very
different from what it appears to have been in earlier periods. Among
other examples, in proof of this assertion, we may notice the
great difference which has taken place in the produce and soil of
Byzacium. This district was formerly much renowned for its fertility;
and we are informed by Pliny that one grain of corn from the Byzacium
was sent to the Emperor Augustus, which yielded four hundred shoots;
and that three hundred and forty stems had been afterwards sent to
Nero, produced equally from a single grain of corn[a]. But whatever
be the cause of the change which has taken place, we find the
soil of the Byzacium to have greatly fallen off from its former
extraordinary fertility; in proof of which we need only extract
the following observations from Shaw’s Travels in Barbary.
“The many parts which I have seen of the ancient Byzacium, or
winter circuit, fall vastly short in fertility of the character
which has been attributed to them by the ancients. For such as
are adjacent to the sea coast are generally of a dry, sandy nature,
with no great depth of soil in the very best portion of them. This is
called the Sahul, and is planted for the most part with olive-trees,
which flourish here in the greatest perfection. Neither is the
inland country in a much better condition.”]
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