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The longest rivers of Central America flow to the Caribbean, and many small streams drain into the Pacific. Longer rivers include the Motagua of Guatemala; the Ulúa, Aguán, and Patuca of Honduras; the Coco, which forms part of the Honduras-Nicaragua boundary; the Río Grande and Escondido of Nicaragua; and the San Juan, which forms a section of the Nicaragua-Costa Rica border. Some of the rivers flowing to the Caribbean are navigable by small craft, but the streams flowing to the Pacific are too steep or too shallow for navigation. Central America has three large lakes—Lake Nicaragua and Lake Managua in Nicaragua and Gatún Lake in Panama. Part of the Panama Canal, a great commercial waterway between the Atlantic and the Pacific, is in Gatún Lake.
Temperatures in Central America, which is situated between the tropic of Cancer and the equator, vary principally according to altitude rather than latitude. Three main temperature zones are discernible. The tierra caliente (“hot country”), which extends from sea level to an altitude of about 915 m (about 3,000 ft), has average yearly temperatures of 24° C (75° F) or more; the tierra templada (“temperate country”), from about 915 to 1,830 m (about 3,000 to 6,000 ft), has a mean annual temperature of 18° to 24° C (65° to 75° F); and the tierra fría (“cold country”), from about 1,830 to 3,050 m (about 6,000 to 10,000 ft), has average yearly temperatures of 13° to 18° C (55° to 65° F). The Caribbean coast and eastern mountain slopes generally receive twice as much annual precipitation as the Pacific coast and western mountain slopes. The relative dryness of the Pacific slope is due to the presence of cold stable air caused by the cold California Current. This current, much like the Peru, or Humboldt, Current along the Peruvian coast, chills the air, thus preventing it from absorbing much water vapor and reducing the possibilities for precipitation. In contrast, the effects of the warm water of the Caribbean Sea allow the air to absorb abundant moisture, which is then carried by the prevailing easterly winds. Much condensation and rainfall occur as the winds flow up and over the high slopes of Central America. Rainfall is greatest along the Mosquito Coast of easternmost Nicaragua—San Juan del Norte receives about 6,350 mm (about 250 in) of rain per year. In October 1998 Hurricane Mitch savaged Central America, killing at least 11,000 people, leaving thousands more missing, and displacing more than two million others. Nicaragua and Honduras absorbed the brunt of the damage, but El Salvador, Guatemala, Belize, and other countries in the region also felt the effects of the storm. Some observers called Mitch the worst natural disaster ever to strike Central America.
Central America is essentially a land bridge uniting two previously isolated ecosystems. As a result, a mixture of both North and South American plant and animal species is found here. The lowland rain forest of the Caribbean and Pacific coasts resembles the selva, or tropical rain forest, of South America. This is especially true below an elevation of about 1,000 m (about 3,280 ft), with large numbers of palms, tree ferns, lianas, and epiphytes (air plants) reflecting the high rainfall and humidity of the region. Vegetation at altitudes of about 1,000 to 1,600 m (about 3,280 to 5,250 ft) shows ties with North America. The pine and oak forests of these highlands are like those of the Mexican highlands. High-altitude regions of Guatemala contain grasses like those of Mexico and the United States, and at about 3,100 m (about 10,170 ft) in Costa Rica are tall grasses similar to those growing above the tree line in the Andes Mountains of South America.
Most of the animal life of Central America is similar to that of South America, but some animals have ties with North America. The marley and opossum have links with South America, as do the jaguar, ocelot, jaguarundi, and margay, which are members of the cat family. In contrast, the puma, gray fox, and coyote are of North American origin. The armadillo, anteater, and sloth have ties to the south, deer to the north. The large manatee, an aquatic plant eater, survives in the isolated lagoons of eastern Central America. Other food sources are the large green turtle and the iguana. Central America provides a habitat for numerous snakes such as the boa constrictor and the bushmaster. Parrots, the quetzal, toucans, and fish are common; notable are the landlocked sharks of Lake Nicaragua.
The minerals of Central America were an early lure for European settlers, especially the gold and silver found in Honduras and the highlands of Nicaragua. In addition, Honduras has significant deposits of lead, zinc, copper, and low-grade iron ore, and Nicaragua has large deposits of natural gas offshore in the Pacific. Large nickel deposits are in the vicinity of Izabal in Guatemala, and the country also has substantial reserves of petroleum, including those near Chinajá. Panama has considerable deposits of copper at Cerro Colorado.
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© 2008 Microsoft
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