gh these agencies that the
revolutionists were so well supplied with arms, ammunition, and other
necessities during the eight years of civil war. While we are writing
these lines, the cable brings us news of a fresh landing of
"filibusters" on the shores in this immediate neighborhood.
Cuba is the most westerly of the West Indian isles, and compared with
the others has nearly twice as much superficial extent of territory,
being about as large as England proper, without the principality of
Wales. Its greatest length from east to west is very nearly eight
hundred miles; its narrowest part is over twenty miles, and its
average width about forty miles. The circumference of the island is
set down at two thousand miles, and it is supposed to contain
thirty-five thousand square miles. The face of the interior is
undulating, with an average level of three hundred feet above the
surface of the sea. The narrow form of the island, and the chain of
mountains which divides it throughout its whole length, leave a
limited course for its rivers, and consequently most of these in the
rainy season become torrents, and during the rest of the year are
nearly dried up. Those streams which sustain themselves at all seasons
are well stocked with fine fish, and afford to lovers of the piscatory
art admirable sport. Near their mouths some of the rivers, like those
of the opposite coast of Florida, are frequented by crocodiles.
The chain of mountains running through the centre of the island, more
or less broken in its course, is lofty in the east, but gradually
diminishes in elevation towards the west, until it becomes a series of
gently undulating hills of one or two hundred feet above sea level,
ceasing as a connected range in the vicinity of Matanzas. On the
easterly end this range of mountains approaches the south coast
between Puerto Principe and Trinidad. The country lying between Cape
Cruz, Cape Maysi, and the town of Holguin has the highest elevations;
the most lofty point, Turquino, lately measured, has a height of ten
thousand eight hundred feet. Illustrative of the great revolutions
which the globe has undergone in its several geological epochs,
petrified shells and bivalves are found on the summits of these
highest peaks, surrounded by coral rocks, both of which differ
entirely from those at present existing on the shores of the Antilles.
An immense bowlder was pointed out to us on the summit of La Gran
Piedra, at an elevation of
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