Part 2—Chapter II.
Central America.
Leaving the continent of North America, which may be said to terminate at the southern end of Mexico, we enter that extremely irregular portion of land which, now widening, now narrowing again, stretches in a south-easterly direction till it unites with the southern half of the American continent at the Isthmus of Panama. We find in Central America three marked centres of elevation. The first we reach is the great plain, nearly 6000 feet above the level of the sea, on which the city of Guatemala is situated. Numerous volcanic peaks rise from its midst; from it also flow several large rivers, some falling into the Gulf of Mexico, others eastward into the Gulf of Honduras, while smaller streams send their waters westward into the Pacific Ocean. The banks of these rivers are mostly covered with the richest tropical vegetation—the scenery of the river Polochie in Guatemala being especially beautiful. Another high plain occupies the centre of Honduras, and extends into the northern part of Nicaragua. From it also rise numberless streams, some emptying themselves into the Caribbean Sea, and others into the Lakes of Nicaragua and Managua. Further south rises the volcano of Cartago. Here the Cordilleras resume their general character of a vast mountain barrier, but once more sink down into low ridges as the chain passes through the Isthmus of Panama.
As in South America, the Cordilleras run close along the Pacific coast. In consequence, the rivers which flow from their heights have a long course on the Atlantic side, and have carried down a large quantity of alluvial soil. Here, too, rain falls in greater or lesser quantities throughout the year. The vegetation is consequently rank, and the climate damp, and proportionately unhealthy. As the trade-winds blow from the north-east, the moisture with which they are saturated is condensed against the mountainsides, and flows backwards towards the Atlantic. The Pacific slope is, therefore, comparatively dry and salubrious—as indeed are also the elevated table-lands of the interior.
The whole region is subject to earthquakes, and numberless volcanoes rise in all directions. In the low ridge which separates the Lake of Nicaragua from the Pacific are several volcanic hills, most of them active; while further to the north-west, in the district of Conchagua—scarcely more than one hundred and eighty miles in length—there are upwards of twenty volcanoes. The two most lofty are found in the Guatemala range—that of Fuego being upwards of 12,000 feet in height, and that of Agua, 18,000 feet.
Many parts of the interior of the country have been but very partially explored, and are, indeed, almost unknown. Of the purely native tribes, most of them have become mingled with Spaniards or negroes. Parts of the coast are inhabited by mixed races of Caribs, who have migrated from Saint Vincent, one of the Leeward islands. These Caribs are
known as the Black and Yellow Caribs—the former being the descendants of the survivors of the cargo of an African slaver, wrecked in the neighbourhood of that island. The descendants of the Spaniards are the dominant race, and they have divided the country into various republics, though the greater portion is still in almost as savage a condition as when first discovered.