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THE MKSSAKIA. IV'.] 73 change ; the soil was red, and we entered the compact grey limestone (Jurassic) which forms the Carpas range. On the extreme verge of the plateau of red soil we had an admirable example of the formation of the conical mounds of earth, two or three of which already existed, while others were in process of development from the melting-away of the soil during heavy rains. As the surface dissolved under the action of rainfall, it flowed down the steep inclinations, until a base was formed, at the expense of the upper area ; by degrees gullies were created in the rear, and these would rapidly become deeper under the action of running water, until they reached the lower level of the base. A circle thus formed, an apex would be the natural result of the denudation and decay of the upper surface which would produce a cone. A sudden shower compelled us to take refuge beneath a caroub-tree whose dense foliage saved us from a thorough soaking. The ground having become slippery, we returned upon our narrow and soapy route with some caution, but the careful animals who were well accustomed to these dangerous paths carried us safely to our camp. It is extraordinary that the water-power of Cyprus has of late years been so neglected by the authorities, as the island must from ancient times have mainly depended upon its springs in the absence of dependable seasons. Kythrea is an example of the importance that was attached to a stream of running water, as the town was established by the Athenians, and in former ages an aqueduct of masonry extended for twenty-five miles to Salamis ; in the neighbourhood of which ruins of the old work are still existing. If the seasons of Cyprus have undergone a change since the forests have been destroyed, I can see no reason for the innumerable

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