An indentation of the coast marks the spot where a slender stream
descends to the sea through a stretch of white sand; and beyond
this the rocky coast rises but slightly above the sea level. Our
steps were directed towards the so-called Cave of Hercules. This
was originally a mere hollow in the face of the sea cliff; but from
a remote period of antiquity it has been quarried for the purpose
of extracting the hand-mills universally used in this part of
Marocco. These, which are quite the same as the Scotch _querns_,
are cut out in the rudest way by hammer and chisel, leaving the
surface of the rock marked by a series of circular indentations about
eighteen inches in diameter. In this way the original dimensions of
the cave have been greatly enlarged, and, as it is still worked for
the same purpose, the process is sure to be continued. In connection
with the question raised of late years as to change of relative
level of land and sea within the historic period, we observed some
very ancient markings that showed the works to have been carried
somewhat below the present level of high tide; but we could trace
none that appeared to reach so low as that of the ebb tide.
So far as the evidence at this point goes, it seems to prove a slight
amount of submergence during the period for which the rock has
here been quarried. This period may probably be reckoned at 2,000
years, and possibly much exceeds that limit. Taken in connection
with still existing remains in Greece, Asia Minor, the Phœnician
coast of Syria, and Egypt, it tends to show that the changes in
the general level of the Mediterranean coasts, indicated by many
geologists, must have proceeded very slowly during the historic
period, and that the more considerable oscillations, that have
undoubtedly occurred near Naples and on the east coast of Sicily,
have been mainly due to the local influence of volcanic action.
The soil near the cave was much mixed with sand carried by the wind,
and the plants seen were chiefly widely diffused species that find
tolerably uniform conditions of life on the sandy shores of the
west coast of Europe. The rocks near the cave produce samphire and
the sea fern (_Asplenium marinum_), just as they do in Cornwall;
while _Diotis maritima_ and _Lotus Salzmanni_, a local variety of
the widely spread _Lotus creticus_ of Linnæus, were frequent on
the sands. The chief ornament was _Statice sinuata_, whose delicate
azure flowers were already in blossom, long before most of the
species of that late-flowering genus.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account