Jamaica, the most valuable of the British possessions in the West
Indies, has an area of 4256 square miles, of which 110,000 acres are
cultivated, chiefly as sugar-plantations. The principal chain of the
Blue Mountains lies in the centre of the island, from east to west, with
so sharp a crest that in some places it is only four yards across. The
offsets from it cover all the eastern part of the island; some of them
are very high. The more elevated ridges are flanked by lower ranges,
descending to verdant savannahs. The escarpments are wild, the
declivities steep, and mingled with stately forests. The valleys are
very narrow, and not more than a twentieth part of the island is level
ground. There are many small rivers, and the coast-line is 500 miles
long, with at least 30 good harbours. The mean summer-heat is 80° of
Fahrenheit, and that of winter is 75°. The plains are often unhealthy,
but the air in the mountains is salubrious; fever has never prevailed at
the elevation of 2500 feet.
Cuba, the largest island in the Colombian Archipelago, has an area of
3615 square leagues, and 200 miles of coast, but so beset with coral
reefs, sandbanks, and rocks, that only a third of it is accessible. Its
mountains, which attain the height of 8000 feet, occupy the centre and
fill the eastern part of the island, in a great longitudinal line. No
island in these seas is more important with regard to situation and
natural productions; and although much of the low ground is swampy and
unhealthy, there are vast savannahs, and about a seventh part of the
island is cultivated.
The Bahama Islands are the least valuable and least interesting part of
the Archipelago. The group consists of about 500 islands, many of them
mere rocks, lying east of Cuba and the coast of Florida. Twelve are
rather large, and are cultivated; and though arid, they produce Campeche
or log-wood and mahogany. The most intricate labyrinth of shoals and
reefs, chiefly of corals, madrepores, and sand, encompass these islands;
some of them rise to the surface, and are adorned with groves of
palm-trees. The Great Bahama is the first part of the New World on which
Columbus landed—the next was Haiti, where his ashes rest.
The geology of Central America is little known; nevertheless it appears,
from the confused mixture of table-lands and mountain-chains in all
directions, that the subterraneous forces must have acted more partially
and irregularly than either in South or North America. Granite, gneiss,
and mica-slate form the substrata of the country; but the abundance of
igneous rocks bears witness to strong volcanic action, both in ancient
and in modern times, which still maintains its activity in the volcanic
groups of Guatemala and Mexico.
Public-domain text, read in full here on John Shaqi.
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