The Path At Length Turned To The Left And Led
Through A Gap That Rounded The Mountain Base, And Formed The Extreme End
Of The Jurassic Limestone, Which Only Exists In Cyprus In The Peculiar
Wall-Like Carpasian Range Running From West To East Upon The Northern
Coast.
We crossed a stream of water at the bottom of the gorge which winds
through the narrow glen that
Terminates the range; and ascending upon
the opposite side, we at once entered upon steep slopes composed of
marls interspersed with an exceedingly bright rose-coloured marble in
veins of about two feet thickness. This would probably develop
considerable blocks if quarried to a greater depth.
Continuing for about two miles along the glen, which was cultivated with
barley in all available localities, we several times crossed the stream
in its winding course, and my dogs hunted the steep myrtle-covered banks
in expectation of game; but nothing moved, and the croaking of numerous
frogs was the only sign of life. The glen now widened to a valley about
a mile and three-quarters in diameter, surrounded upon all sides by
heights, and we commenced one of the steepest ascents in Cyprus, up the
face of the slope about 1000 feet above the bottom. The zigzags were
upon a surface of white marl, which during wet weather would become as
slippery as soap, and be impassable for loaded animals. Many times our
mules were forced to halt and rest, but they were good and sure-footed
beasts, that could always be depended upon.
At length we gained the summit, which was a total change of scene.
Instead of descending upon the other side, as I had expected, we had
arrived at a plateau eight or nine miles in length from north to south,
and an invisible distance from east to west. The soil was a rich reddish
chocolate, forming a grateful contrast to the glaring white marls that
we had just quitted, and which composed the steep hills that surrounded
the lower basin. A growth of young pines and other evergreen shrubs
ornamented the surface, and at about a quarter of a mile from the summit
of the pass by which we had arrived we halted at a well of pure water
among a small grove of olive-trees. Although we were at least 1000 feet
above the valley, the water was only ten feet from the coping-stone by
measurement. There could be little doubt that the perennial stream in
the deep glen was the result of the drainage of this extensive
table-land, corresponding with similar heights upon the other side.
Having breakfasted by the well of deliciously cold water, we remounted,
and continued our route along the extensive table-land. This was
cultivated in many places, but as we advanced for two or three miles the
country became exceedingly wild, and we entered a wood of Pinus
maritima, composed of young trees of several years' growth, and older
stems that had been mutilated in the disgraceful manner that
characterises all Cyprian forests.
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