Honduras | History, Geography, & Culture (2024)

Relief

More than three-fourths of the land area of Honduras is mountainous, lowlands being found only along the coasts and in the several river valleys that penetrate toward the interior. The interior takes the form of a dissected upland with numerous small peaks. The main surface features have a general east-west orientation. There is a narrow plain of alluvium bordering the Gulf of Fonseca in the south. The southwestern mountains, the Volcanic Highlands, consist of alternating layers of rock composed of dark, volcanic detritus and lava flows, both of middle to early Cenozoic age (i.e., about 2.6 to 65 million years old). The northern mountains in other regions are more ancient, with granite and crystalline rocks predominating.

Four geographic regions may be discerned:

1. The eastern Caribbean lowlands (including the northern part of the Mosquito [Miskito] Coast, called La Mosquitia) and mountain slopes embrace about one-fifth of the total land area of Honduras. Hot and humid, this area is densely forested in the interior highlands, and lumbering is an important economic activity. Subsistence agriculture and fishing are the main support of the scattered population.

2. The northern coastal and alluvial plains and coastal sierras make up about one-eighth of the land area and contain about one-fourth of the population. This is an economically important region, the clayey and sandy loam soils producing rich crops of bananas, rice, cassava (manioc, or yuca), oil palm, corn (maize), citrus fruits, and beans. Cattle, poultry, and pigs are raised. The nation’s railroads are confined to this northern area, which has four of the five important ports of entry.

3. The central highlands take up two-thirds of the national territory and contain the vast majority of the population. The mountains are rugged, rising in the west to 9,347 feet (2,849 metres) at Mount Las Minas, the highest point in the country. The numerous flat-floored valleys lie between 2,000 and 4,000 feet (600 to 1,200 metres) in elevation. The generally fertile soils, derived from lava and volcanic ash, produce coffee, tobacco, wheat, corn, sorghum, beans, fruits, and vegetables and support cattle, poultry, and pigs.

4. The Pacific lowlands, centred on the Gulf of Fonseca, and the adjacent lower mountain slopes are only a small part of the land area and contain an equally small part of the population. The fertile soils, composed of alluvium or volcanic detritus, produce sesame seed, cotton, and some corn and sorghum. Cattle are raised on the lowland pastures, and coffee is grown on the nearby uplands.

Climate

The climate is generally hot, with high humidity in the tropical coastal lowlands becoming modified by elevation toward the interior. Lowlands below 1,500 feet (460 metres) have mean annual temperatures between 79 and 82 °F (26 and 28 °C). The north coast is occasionally affected from October to April by cool northern winds of continental origin. Mountain basins and valleys, from 2,000 to 4,000 feet (600 to 1,200 metres), have mean annual temperatures of 66 and 73 °F (19 and 23 °C). At Tegucigalpa, located on hilly terrain at an elevation of 3,200 feet (975 metres), the rainy season starts in May and continues until mid-November, with temperatures sometimes reaching 90 °F (32 °C) in May and dropping to 50 °F (10 °C) in December, the coolest month. Around 7,000 feet (2,100 metres) mean annual temperatures are about 58 °F (14 °C). In the northern and eastern coastal and alluvial plains and on adjacent mountains, mean annual precipitation ranges from 70 to 110 inches (1,800 to 2,800 mm) or more, with a less rainy season from March to June; these areas occasionally have summer hurricanes that are accompanied by heavy rains. Pacific plains and mountain slopes get 60 to 80 inches (1,500 to 2,000 mm) of rain annually but from December to April receive little or no rain. Interior sheltered mountain basins and valleys receive 40 to 70 inches (1,000 to 1,800 mm) annually.