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SIR SAMUEL WHITE BAKER
CYPRUS AS I SAW IT IN 1879
page 93 View PDF version of this page resemble volcanic cones. W e rode up precipitous paths edging upon deep chasms between these conical hills, and emerged upon metamorphous rocks and shale mingled in curious irregularity. The strata of shale Avere in some instances nearly vertical, proving the disturbance that had been occasioned by a subsequent upheaval. About 200 feet above this formation we entered upon the dark grey Jurassic limestone, and the soil became a rich red like that of South Devon. The rock scenery was very imposing as we increased our altitude and arrived upon plateaux of considerable extent. There can be no doubt that these natural terrace-like surfaces and various hollows accumulate the rainfall of a great area, and that some vast subterranean caverns in the limestone form natural reservoirs, which supply the celebrated springs of Kythrea throughout the year. "
I believe these few words contain the real secret of the springs, which have been, and still are, considered to have a mysterious origin. Some people indulge in the theory that the water is forced by hydraulic pressure at the superior altitude of Caramania in Asia Minor, and passing by a subterranean conduit far beneath the bottom of the intervening channel, it as cends at the peculiar rock-mouth of Kythrea. This is simple nonsense, and can only be accepted by those who adore the unreal, instead of the guide, " commonsense. " The actual volume of the outflow at Kythre has never been calculated, although the problem is most simple ; but a cursory examination is sufficient to explain the origin of the supply which a certain superficial mountain area collects and stores during the rainy seasons : to yield gradually through some small aperture or leak in a grand subterranean reservoir.
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