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vorite Domestic Product.--Milk Supply.--Prolific Sheep. --A Maltese Market.--Quail Shooting.--Rabbato, Capital of Gozo.--The Old Citadel.--Lace Manufacture.--Prehistoric Ruins.--The Giant's Tower.--Attractive Summer Resort.--Pagan Worship. Gozo, the fabled isle of Calypso, the Gaulos of the Greeks, the Gaulum of the Romans, and the Ghaudex of the Arabs, with its rock-bound, cave-indented shores, is oval in shape, and has the same general characteristics as Malta, but is much more fertile. The undulating surface of the island gives a casual observer the idea of its being a hilly country, yet at only one place does it reach a height of over three hundred feet above sea-level. This is at Dibiegi, where a hill rises to an elevation of about seven hundred feet. When approached from the sea, Gozo appears to lie much lower than Malta proper, and this is really so. Through the early morning haze, both look like huge marine monsters sleeping upon the surface of the waters. The hills we have referred to are singularly conical, but are uniformly flattened at their tops by the disintegrating process of the elements, causing them to present the appearance of a myriad little volcanoes, though they are very innocent of any such dreaded association. In the Hot Lake District of New Zealand, near Ohinemutu, the author has seen a precisely similar appearance, but in the latter instance the effect was undoubtedly produced by volcanic action. The boiling springs, geysers, and hot lakes of this New Zealand district are almost identical in character with our Yellowstone Park phenomena. Both must be the result of smouldering fires far below the surface of the earth. In the New Zealand district an active volcano is near at hand, which often rages with destructive force. Gozo is beautified with occasional groves of trees, which is an adornment almost entirely wanting in the larger island. These groves, however, are by no means numerous. The one great deficiency of the group is the absence of arboreal vegetation, and yet an abundance of trees could be made to grow and flourish here with very little effort. There are marl beds which might be utilized for the purpose, situated in various parts of the islands, besides which, the rocky formation of the group, as we have shown, is of a porous nature, full of fissures and crevices, easily admitting the roots of vegetation. There is a tradition that Malta was once covered w
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