I | INTRODUCTION |
Central
America, region of the western hemisphere, made up of a long, tapering
isthmus that forms a bridge between North and South America. Central America,
which is defined by geographers as part of North America, has an area of about
521,500 sq km (about 201,300 sq mi) and includes the countries of Guatemala,
Belize, El Salvador, Honduras, Nicaragua, Costa Rica, and Panama. The region has
a population of approximately 36.4 million (2000 estimate).
II | THE NATURAL ENVIRONMENT |
In strictly geological terms, Central America
begins at the narrow Isthmus of Tehuantepec, in southern Mexico. That narrow
section divides the volcanic rocks to the northwest from the folded and faulted
structures of Central America. The southernmost geological limit of Central
America is the Atrato River valley, in Colombia, South America, just east of the
Panama border.
A | Geologic History |
Central America, a particularly unstable
region of the earth’s crust, is on the western edge of the Caribbean plate
(see Plate Tectonics). Subduction of oceanic crust beneath this edge,
beginning in the Miocene Epoch, about 25 million years ago, has lifted the land
from the sea. In the earliest stage, a peninsula and archipelago formed. Later,
about three million years ago, the scattered islands coalesced to form a true
land bridge, or isthmus, linking North and South America.
Keeping pace with subduction and uplift have
been volcanic eruptions—Central America has at least 14 active volcanoes—and
frequent earthquakes. In this century alone, Managua, the capital of Nicaragua,
has twice been destroyed by earthquakes. The most recent, in 1972, took 10,000
lives. In 1976 some 25,000 people were killed in an earthquake registering 7.5
on the Richter scale and centered in the Motagua depression in Guatemala. This
quake left 25 percent of the country’s population homeless. Volcanic activity
has produced a landscape dotted with majestic cones built from eruptions of ash
and lava, and beautiful lakes formed in collapsed volcanic craters called
calderas.
B | Natural Regions |
For the most part Central America is a
rugged, mountainous area, with 109 large volcanoes, some more than 4,000 m
(13,000 ft) high; Tajumulco Volcano, in Guatemala, is the highest at 4,220 m
(13,845 ft). Central America is one of the most active volcanic zones in the
western hemisphere. The land surface slopes up rather abruptly from a narrow
coastal plain along the Pacific Ocean to the mountain crests, and then descends
more gradually to a broader plain along the Caribbean Sea. Two major
interoceanic passes cut through the highlands of Central America, one in
Nicaragua (from the mouth of the San Juan River to Lake Nicaragua) and the other
in Panama (along the route of the Panama Canal). The Pacific coastline is about
2,830 km (about 1,760 mi) long, and the Caribbean coastline is approximately
2,740 km (approximately 1,700 mi) long. Several groups of small islands lie off
the Caribbean coast, and some of them, such as the Bay Islands (Islas de la
Bahía) in the Gulf of Honduras, are inhabited.
C | Rivers and Lakes |
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.
D | Climate |
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.
E | Vegetation |
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.
F | Animal Life |
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.
G | Mineral Resources |
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.
III | THE PEOPLE |
Most of the inhabitants of Central America
live on the Pacific side of the isthmus, where they occupy both lowland and
highland environments. The rainy, forested Caribbean slope and coast are
sparsely settled.
A | Ethnography |
A substantial majority of the people of
Central America are Native Americans or mestizos (people of mixed
heritage, chiefly of Spanish and Native American descent). Along the narrow
Caribbean coast blacks and mulattoes (people of mixed white and
black-African backgrounds) predominate. About half of the people of Belize are
of black-African or partly black-African ancestry. The great majority of Costa
Ricans are of unmixed Spanish background, and approximately 90 percent of the
inhabitants of El Salvador and Honduras are of mixed Spanish and Native American
descent. About 45 percent of Guatemalans are Native Americans, and mestizos make
up most of the rest of the country’s population. About 70 percent of Nicaragua’s
and Panama’s inhabitants are mestizos. Panama has a sizable black minority. In
general, the Native American element is less apparent in the southern countries
of Nicaragua, Costa Rica, and Panama.
B | Demography |
The population of Central America is
concentrated in districts of dense settlement, separated by areas of sparse
habitation. Population densities reach more than 385 persons per sq km (more
than 1,000 per sq mi) in parts of the Meseta Central of Costa Rica, but vast
areas of eastern Honduras and Nicaragua have fewer than 4 persons per sq km
(fewer than 10 per sq mi). The rate of population increase in much of Central
America is high; in 2008 Nicaragua had an annual growth rate of 1.82 percent;
Guatemala, 2.11 percent; Costa Rica, 1.38 percent; and Panama, 1.53 percent. The
population increase is principally the result of continuing high birth rates and
falling death rates. Increasing political unrest, economic hardship, guerrilla
warfare, and military repression have forced many rural residents into urban
centers; thousands also decided to begin the long trek to the United States via
Mexico.
The people of Central America are
becoming increasingly urbanized. In the mid-1990s about 45 percent of the
inhabitants of El Salvador and Honduras and about 40 percent of Guatemalans were
considered urban, while more than half the people of Panama and nearly
two-thirds of Nicaragua’s people lived in urban areas. In each country except
Belize the national capital is the largest city; the biggest urban center of
Belize is Belize City.
C | Language and Religion |
Spanish is the official language of all
Central American countries except Belize, where English is the language of
government. Many highland Native Americans use traditional languages, such as
Quiché, Mam, and Kekchí in Guatemala, and Chortí in Honduras. Some Native
Americans also speak Spanish as well. Roman Catholicism is by far the dominant
religion of Central America although Evangelicalism, Methodism, and Mormonism
are making increasingly significant inroads in Costa Rica, Honduras, and
Panama.
D | Cultural Activity |
Cultural patterns in Central America are
based largely on the heritage of the Maya and other Native Americans and of the
Spanish colonial period. Considerable change has occurred in the region’s
cities, however, where the mass media and modern cultural institutions have much
influence. The countries of Central America have established many educational
facilities, but a comparatively large proportion of the children do not attend
school. Although the great majority of people aged 15 and over in Costa Rica and
Panama are literate, this figure drops to three-quarters in El Salvador and
Honduras, about two-thirds in Nicaragua, and just over one-half in Guatemala.
IV | PATTERNS OF ECONOMIC DEVELOPMENT |
In the early 1990s the countries of Central
America had relatively undeveloped economies in which agriculture was the most
important sector. Manufacturing largely involved processing raw materials. The
annual per capita income was low.
A | Agriculture |
Farming is by far the leading economic
activity in Central America. The principal cash crops, such as coffee, bananas,
sugarcane, and cotton, are typically produced on large landholdings, and a
substantial proportion are exported, mainly to the United States and Europe.
Food for local consumption is raised mainly on small farms; most of it is
consumed by the farm families, and relatively little is marketed. The chief
subsistence food commodities are corn, beans, bananas, manioc, rice, and
poultry. Cattle are raised on big ranches located mainly in the drier regions of
western Central America. Modern farming methods are used on the large
landholdings, but the small farmers generally use relatively simple techniques
that hold down productivity.
B | Forestry and Fishing |
About 40 percent of Central America is
forested. The early years of European activity in Belize, for example, revolved
around the extraction of dyewoods, and later mahogany, chicle, and pine timber
were produced. British timber companies also cut mahogany and cedar along the
greater Caribbean coast. Today, forestry is a relatively unimportant aspect of
the Central American economy. Pine is the main wood harvested, and some
hardwoods, such as cedar, mahogany, and rosewood, also are cut.
Fishing too is a comparatively minor
economic activity in Central America. Shrimp and spiny lobster, caught off the
coasts of Belize, El Salvador, and Panama, are mostly exported to the United
States. Since the mid-1960s Panama has developed a fish-meal and fish-oil
industry. Central America has a low rate of per capita fish consumption.
C | Mining |
The mineral output of Central America is
small. El Salvador, Honduras, and Nicaragua produce limited quantities of
silver, gold, lead, copper, and antimony. In the early 1980s Guatemala began to
export small quantities of crude oil.
D | Manufacturing |
Most of the manufacturing plants of
Central America process raw materials of the region such as sugarcane, coffee,
cotton, timber, and fish. In addition, since the 1950s a concerted attempt has
been made to reduce the need to import basic fabricated articles. Thus,
factories making paint, detergents, tires, paper and cardboard articles,
fertilizer, and insecticide have been established in the major urban areas.
Many manufacturing establishments in
Central America involve only a handful of workers, and few employ more than 10
people. Large-scale manufacturing is hindered by the region’s lack of energy
sources, its undeveloped transportation systems, and its small markets.
E | Energy |
About half of the electricity of Central
America is generated by hydroelectric installations; important dams include
those on the Lempa River in El Salvador, the Cajón River in Honduras, and the
Corobicí and Arenal rivers in Costa Rica. Most of the rest is produced in plants
using petroleum products. A small amount is generated in wood-burning
facilities.
F | Transportation |
The mountains of Central America present a
major obstacle to overland transport, and the only surface transportation artery
linking all the countries of the region is a section of the Pan-American
Highway. Railroads connect the Caribbean and Pacific coasts in Guatemala, Costa
Rica, and Panama. Inland water transportation is of little economic importance,
but Central America has several important seaports, such as Puerto Santo Tomás
de Castilla and Puerto San José in Guatemala; Puerto Cortés in Honduras;
Acajutla in El Salvador; Corinto in Nicaragua; Puerto Limón in Costa Rica; and
Bahía las Minas in Panama. The Panama Canal is a major shipping link between the
Atlantic and Pacific oceans; Panama took over its operation from the United
States in 1999. A crude-petroleum pipeline across western Panama was completed
in 1982. Airlines provide transportation among the big cities of Central America
and serve some remote mountain communities.
G | Foreign Trade |
About half of Central America’s
intercontinental trade is with the United States and Canada. Almost all the rest
is with Western Europe, Mexico, and countries of South America. Central
America’s principal imports are manufactured goods, such as motor vehicles, farm
machines, textiles, electrical equipment, processed food, chemicals, and
pharmaceuticals. The main Central American exports are basic commodities, which
include bananas, coffee, cacao, meat, chicle, cotton, mahogany, balsa, hides and
skins, and rubber.
The Central American Common Market (CACM),
established in 1960, included all the Central American countries except Panama
and Belize. However, several circumstances kept it from achieving its goals of
trade liberalization and the establishment of a free-trade area. Among these was
the infamous “Soccer War” of 1969 between El Salvador and Honduras, caused in
part by CACM rules that favored El Salvador as well as Honduran policies against
migrant Salvadoran workers. As a result, CACM trade was affected for more than a
decade. Other countries’ internal conflicts also played a role in the
disturbance of trade and by 1970, intra-CACM trade was insignificant. Today,
Central American countries are facing new tariff barriers as the result of the
Caribbean Basin Initiative (1984) and the North American Free Trade Agreement
(NAFTA) (1994) and these barriers are preventing them from benefiting from
increased global trading patterns.
V | HISTORY |
The region between Mexico and Colombia
supported a large pre-Columbian population, the most important of whom were the
Maya. The Maya civilization originated in the highlands of Guatemala before the
1st millennium bc and reached its
greatest flowering between ad 300
and 900 in autonomous city-states in what are now northern Guatemala, Honduras,
Belize, and Mexico’s Yucatán Peninsula. Maya unity was cultural rather than
political, but the civilization’s influence was widespread. Maya artistic and
scientific achievements surpassed those of contemporary Europeans. After 900,
however, the Maya civilization declined, and its people came under the influence
of Toltec people from Mexico.
Numerous peoples inhabited the remainder of
the isthmus and traded with both South and North American tribes, making ancient
Central America an archaeological bridge between the Americas. The population of
the isthmus on the eve of the Spanish conquest may have been as large as six
million, a figure not again achieved until the 20th century.
A | The Colonial Period |
Christopher Columbus established Spain’s
claim to Central America in 1502, when he sailed along its coast from the Gulf
of Honduras to Panama. His reports of great wealth beyond the mountains that ran
the length of the heavily populated isthmus stimulated Spanish conquest, which
was launched from Hispaniola under Columbus’s son, Diego. The charismatic Vasco
Núñez de Balboa founded Spain’s first truly productive colony in America at
Darién in 1510, and went on to reach the Pacific Ocean in 1513. His successor,
Pedrarias Dávila, who ordered Balboa’s death in 1517, extended the colony
considerably, founding Panama City in 1519, from which he initiated the
subjugation of Nicaragua and Honduras. The subsequent conquest of Central
America became a bloody struggle among Spaniards representing interests in
Panama, Hispaniola, and Mexico. Eventually, Pedro de Alvarado, the loyal
lieutenant of the conqueror of Mexico, Hernán Cortés, consolidated control over
most of the isthmus. The conquerors killed many Native Americans, but the
majority died from devastating epidemics of smallpox, plague, dysentery, and
influenza, introduced by the Europeans. The Spanish reduced to serfdom those who
remained, establishing an agricultural society based on institutions they had
brought from Spain. Native American customs and traditions survived, however,
because most of the relatively few Spaniards remained in the towns and
cities.
Colonial Central America was divided into
two jurisdictions. The captaincy general of Guatemala extended from Chiapas
(present-day Mexico’s southernmost state) through Costa Rica. Although nominally
part of the Viceroyalty of New Spain, it was relatively autonomous. Its capital
city, Antigua Guatemala, became a center for bureaucrats, clerics, and the
landholding and commercial elite of the colony. The rest of Central America (all
of what is present-day Panama), with its important transit route, became
attached to New Granada (modern Colombia) in the Viceroyalty of Peru.
Spanish decline during the 17th century
permitted increased autonomy for the colonial elite who, with the cooperation of
church and state, dominated the oppressed Native American and mestizo (mixed
Spanish-Native American heritage) working class. In the 18th century Spain’s
Bourbon kings, trying to regenerate the empire, inaugurated reforms that
promoted new economic activity, but also challenged the longtime accommodation
between the landholding elite and the bureaucracy.
B | Federation |
The Creole elite in the captaincy general
of Guatemala followed Mexico’s lead and severed its allegiance to Spain in 1821.
The area then became part of the Mexican Empire of Agustín de Iturbide, but when
Iturbide’s conservative government fell in 1823, liberals seized control,
declared independence from Mexico, and formed the United Provinces of Central
America. Chiapas, however, remained with Mexico, and Panama joined the Republic
of Colombia (also known as Gran Colombia), headed by Simón Bolívar.
The United Provinces embarked on an
ambitious but unrealistic program of republican reform and economic development,
rejecting the Spanish heritage. Intense regionalism, political intrigue among
the elite, and civil war resulted. In 1834 the liberals moved the capital from
Guatemala to El Salvador, but their policies still faced bitter opposition and
rebellion from conservative members of the elite and the rural masses. After the
Guatemalan peasant leader Rafael Carrera captured Guatemala City in 1838, the
federation began to disintegrate; the federal president, Francisco Morazán,
finally resigned in 1840. Guatemala, Honduras, El Salvador, Nicaragua, and Costa
Rica emerged as independent, conservative republics.
C | The Central American Republics |
England, by this time, had replaced Spain
as the dominant external force in the region. The British settlement at Belize
had grown from a buccaneering and logging camp in the 17th century to become the
principal port of Central America’s foreign trade. British influence extended
along the Caribbean coast as far as Panama, and in 1862, Belize officially
became a British colony (British Honduras). United States interest, however,
rivaled British interest after 1849, for the isthmus offered the quickest routes
to the gold mines of California. The Clayton-Bulwer Treaty of 1850 resolved some
areas of this Anglo-American conflict, but in 1855 William Walker, a U.S.
soldier of fortune, invaded Nicaragua with an army of followers. A united
Central American conservative army drove him out with British assistance in
1857. Meanwhile, the completion of the Panama Railroad in 1855 caused Central
American commerce to shift away from Belize to the more accessible Pacific coast
ports, and British influence receded thereafter.
After 1870 liberal dictatorships arose
which, in the name of order and progress, promoted the development of coffee as
the region’s main export; at the expense of a more diversified agriculture,
banana cultivation, mostly controlled by foreign interests, also became
important. After 1900, the U.S.-based United Fruit Company was a major force in
Central America’s economy. Developing railroads, shipping, and other subsidiary
interests, the company was known as the “Octopus” among resentful Central
Americans. U.S. investment and government became the dominant force on the
isthmus, beginning with the establishment of Panamanian independence in 1903.
The United States helped form the Central American Court of Justice, but U.S.
military occupation of Nicaragua from 1912 to 1933 undermined its
effectiveness.
Economic growth in the 20th century
produced new middle classes that began to challenge the continued rule of
traditional elites. Beginning in Costa Rica, reformist and revolutionary parties
had emerged in every country by the middle of the century.
The second half of the 20th century has
seen persistent poverty, political instability and social injustice in many of
the Central American republics still undergoing modernization. In Nicaragua, the
Sandinista guerrilla movement overthrew the Somoza dynasty in 1978 and 1979. The
United States then became involved in a major effort to support the
counter-revolutionary (“contra”) forces against the leftist Sandinista
government, leading to many deaths and great suffering on both sides. El
Salvador’s people and economy were ravaged by civil war through the 1980s.
Guatemala witnessed 36 years of fighting between alleged left-wing groups and a
repressive military. Thousands of people were killed and hundreds of thousands
migrated to escape this conflict, which ended with the signing of a peace
agreement in December 1996. Political repression and corruption in Panama
prompted the United States to intervene in 1989 to remove Panamanian leader
Manuel Noriega, who was allegedly connected to Colombian drug cartels.
One of the most significant problems
confronting all Central American countries is the difficulty of bringing about
significant socioeconomic development without affecting the democratic rights of
their populations. Given its geostrategic significance (especially because of
the Panama Canal and U.S. military bases, which reverted to Panamanian control
in 1999), Central America is inevitably a key zone for U.S. foreign policy. In
the past, political stability has often been allowed to outweigh democratic and
human rights. With the formation of new hemisphere-wide trading blocks, Central
America may find itself once again left behind in the competitive Latin American
struggle to achieve true development.
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