The Story of MaltaBallou, Maturin M. (Maturin Murray)
History
The Story of Malta
Ballou, Maturin M. (Maturin Murray)
Malta -- History
To reach Gozo from Valletta, a boat taken at Quarantine Harbor will land
the visitor at the shallow bay of Migiarro, on the southeastern
extremity of the island, amid a fleet of fishing-boats, hauled high and
dry upon the shelving strand. The boats are called _speronari_, and are
as buoyant and fleet as a sea-bird flying before the wind. They are
pointed at both ends, the prow terminating at a height of two feet above
the level of the thwarts. They have retained their peculiar shape for
centuries. It is always interesting to pause here for a few moments, to
take note of the abundance and excellence of the fish brought in by the
boatmen just arrived from their early morning excursion offshore. The
variety and redundancy of aquatic life in this latitude is something
marvelous.
CHAPTER VI.
Homer's Fabled Siren.--Singular Topographical Formation in
Gozo.--Beautiful Island Groves.--Fertile Grain-Fields.--
Flowering Hedges.--Aromatic Honey.--Herds of Goats.--A
Favorite 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.
Public-domain text, read in full here on John Shaqi.
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