roadsteads for all classes, and could easily be arranged to protect small trading-vessels; while Baffo would, like Kyrenia and Soli, be restored to its original position. All rudimentary harbour-works would be planned with a view to future extension, as might be rendered necessary by the development of trade. Colonel White, 1st Royal Scots, who had been appointed chief commissioner of the Lefkosia district from his former similar position at Larnaca, arrived at Caravastasi upon the same day as ourselves. This very painstaking and energetic officer was exploring his district and investigating all the nooks and corners of the mountainous frontier which bounded his authority; he was accordingly assailed with complaints and lamentations concerning the endless water disputes among the villages; those of the lower ground declaring that the streams to which they were entitled by the rights of centuries had been diverted to other channels, that the Turkish authorities had been bribed by the opposing litigants; with the usual long list of grievances, the discussion of which I shall defer to a special chapter upon "Irrigation." CHAPTER VIII. ROUTE TO BAFFO. Our tent was pitched upon rising ground, which formed the direct slope from the sea, a quarter of a mile distant, to the mountain-top about 1500 or 2000 feet above us; the insignificant village of Caravastasi was upon the sea-beach in our immediate front. From our commanding position I had observed a peculiar mound with a cliff-face half a mile to the west, which exhibited the unusual colour of a bright lemon yellow in close conjunction with red of various shades. Upon crossing numerous fields of barley, which the reapers had just attacked (14th April), I descended a ravine at the foot of this peculiar formation, which I carefully examined. Since we had crossed the plain of Morphu and quitted the compact limestone of the Carpas range we had entered upon an interesting geological change. Eruptive rocks had burst through the marls and calcareous sedimentary limestone of the coast and had produced very curious examples of metamorphous rocks, where the marls and limestone had been in immediate contact with the plutonic. The cliff above me was about fifty feet high, as I stood at its base within a shallow gorge that formed a brook during the rainy season.