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and syenite predominated, with extremely large crystals of hornblende in the latter rock, that would have afforded handsome slabs had not the prevailing defect throughout Cyprus rendered all blocks imperfect through innumerable cracks and fissures. A peculiar greenish and greasy-looking rock resembling soapstone was occasionally met with in veins, and upon close examination I discovered it to be the base of asbestos. Th e surface of this green substance was like polished horn, which gradually became fibrous, and in some specimens developed towards the extremity into the true white hairy condition of the well-known mineral cotton. W e were near the summit of the mountain, and arrived at an ancient camp that had been arranged with considerable judgment by a series of stone walls with flanking defences for the protection of each front. This was many centuries ago the summer retreat of the Venetian government, and it had formed a sanatorium. This extends to the summit of the mountain, where fragments of tiles denote the former existence of houses. In the absence of water it would have been impossible to adopt the usual custom of mud-covered roofs, therefore tiles had been carried from the low country. It is supposed that the stations fell into decay at about the period of the Turkish conquest. A rattle of loose stones upon the opposite side of a ravine suddenly attracted my attention ; and two moving objects at about 230 yards halted, and faced us in the usual manner of inquiry when wild animals are disturbed to windward of their enemy. The rocks were bare, and their cafê-au-lait colour exactly harmonised with that of the two moufflon, which li Β 2

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