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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