|• Total||22,966 km2 (8,867 sq mi)|
|Coastline||386 km (240 mi)|
|Borders|| Total land borders:|
Guatemala 266 km,
Mexico 276 km
|Highest point||Doyle's Delight|
|Lowest point|| Caribbean Sea |
|Longest river|| Belize River |
|Largest lake||New River Lagoon|
|Exclusive economic zone||35,351 km2 (13,649 sq mi)|
Belize is a small Central American nation, located at 17°15' north of the equator and 88°45' west of the Prime Meridian on the Yucatán Peninsula. It borders the Caribbean Sea to the east, with 386 km of coastline. It has a total of 542 km of land borders—Mexico to the north-northwest (272 km) and Guatemala to the south-southwest (266 km). Belize's total size is 22,966 km², of which 22,806 km² is land and 160 km² is water.
Belize is the only country in Central America without a Pacific coastline. Many coral reefs, cays, and islands to the east—such as Ambergris Caye, Lighthouse Reef, Glover's Reef, and the Turneffe Islands—are part of Belize's territory, forming the Belize Barrier Reef, the longest in the western hemisphere stemming approximately 322 km (200 mi) and the second longest in the world after the Great Barrier Reef. Belize's largest river is the eponymous Belize River. Belize's lowest elevation is at sea level. Its highest point is Doyle's Delight at 1,124 m (3,688 ft).
The climate in Belize is tropical, with a rainy season from June to November and a dry season from January to May. Natural hazards include hurricanes (mostly in the late Atlantic hurricane season, September to December) and coastal flooding, especially in the south.
Topographical feature divide the Belizean landscape into two main physiographic regions. The most visually striking of these regions is distinguished by the Maya Mountains and the associated basins and plateaus that dominate all but the narrow coastal plain in the southern half of the country. The mountains rise to heights of about 1,100 metres, with the highest point being Doyle's Delight (1,124 m) in the Cockscomb Range, a spur of the Maya Mountains in Western Belize. Covered with shallow, highly erodible soils of low fertility, these heavily forested highlands are very sparsely inhabited.
The second region comprises the northern lowlands, along with the southern coastal plain. Eighteen major rivers and many perennial streams drain these low-lying areas. The coastline is flat and swampy, with many lagoons, especially in the northern and central parts of the country. Westward from the northern coastal areas, the terrain changes from mangrove swamp to tropical pine savanna and hardwood forest.
Belize claims an exclusive economic zone of 35,351 km2 (13,649 sq mi) with 200 nautical mile s (370.4 km; 230.2 mi) and a territorial sea of 12 nautical miles (22.2 km; 13.8 mi). From the mouth of the Sarstoon River to Ranguana Cay, Belize's territorial sea is 3 nmi (5.6 km; 3.5 mi); according to Belize's Maritime Areas Act, 1992, the purpose of this limitation is to provide a framework for the negotiation of a definitive agreement on territorial differences with Guatemala.
Belize is the only country in Central America without a coastline on the North Pacific Ocean.
The interlocking networks of rivers, creeks, and lagoons have played a key role in the historical geography of Belize. The largest and most historically important river is the Belize River, which drains more than one-quarter of the country as it winds along the northern edge of the Maya Mountains across the center of the country to the sea near Belize City. Also known as the Old River, the Belize River is navigable up to the Guatemalan border and served as the main artery of commerce and communication between the interior and the coast until well into the twentieth century.
Other historically important rivers include the Sibun River, which drains the northeastern edge of the Maya Mountains, and the New River, which flows through the northern sugar-growing areas before emptying into Chetumal Bay. Both of these river valleys possess fertile alluvial soils and have supported considerable cultivation and human settlement.
Belize has a tropical climate with pronounced wet and dry seasons, although there are significant variations in weather patterns by region. Temperatures vary according to elevation, proximity to the coast, and the moderating effects of the northeast trade winds off the Caribbean. Average temperatures in the coastal regions range from 24 °C (75 °F) in January to 27 °C (81 °F) in July. Temperatures are slightly higher inland, except for the southern highland plateaus, such as the Mountain Pine Ridge, where it is noticeably cooler year round. Overall, the seasons are marked more by differences in humidity and rainfall than in temperature.
Average rainfall varies considerably, ranging from 1,350 millimeters (53.1 in) in the north and west to over 4,500 millimeters (177.2 in) in the extreme south. Seasonal differences in rainfall are greatest in the northern and central regions of the country where, between January and April or May, fewer than 100 millimeters (3.9 in) of rain fall per month. The dry season is shorter in the south, normally only lasting from February to April. A shorter, less rainy period, known locally as the "little dry," usually occurs in late July or August, after the initial onset of the rainy season.
Hurricanes have played a devastating role in Belizean history. In 1931 an unnamed hurricane destroyed over two-thirds of the buildings in Belize City and killed more than 1,000 people. In 1955 Hurricane Janet leveled the northern town of Corozal. Six years later, Hurricane Hattie struck the central coastal area of the country, with winds in excess of 300 kilometers per hour (186 mph) and 4-meter (13.1 ft) storm tides. The devastation of Belize City for the second time in thirty years prompted the relocation of the capital some 80 kilometers (50 mi) inland to the planned city of Belmopan. A hurricane that devastated Belize was Hurricane Greta, which caused more than US$25 million in damages along the southern coast in 1978.
There was a period of 20 years that Belize was considered as a hurricane-free zone by many until Hurricane Mitch (October 1998) caused quite a stir and gave rise to hurricane awareness and the National Emergency Management Organization (NEMO). Two years later Tropical Storm Chantal and Hurricane Keith did much to put the country on the hurricane map.
In 2001, Hurricane Iris swept through the southern part of Belize causing damage that ranged in the hundreds of millions due largely to wiping away the banana industry, crippling the citrus and tourism in the area. Six years later, the fury of Category Five Dean landed on the Yucatán coast at Mahahual and Corozal in northern Belize, was not spared the brunt of reportedly Category 3 to 4 winds. Hurricane Dean did tens of millions in damages, especially to the infantile papaya industry and to a lesser extent to the endemic sugar cane industry.
Belizean geology consists largely of varieties of limestone, with the notable exception of the Maya Mountains, a large uplifted block of intrusive Paleozoic granite and sediments running northeast to southwest across the south-central part of the country. Several major faults rive these highlands, but much of Belize lies outside the tectonically active zone that underlies most of Central America. During the Cretaceous Period, what is now the western part of the Maya Mountains stood above sea level, creating the oldest land surface in Central America, the Mountain Pine Ridge plateau.
The hilly regions surrounding the Maya Mountains are formed from Cretaceous limestone. These areas are characterized by a karst topography that is typified by numerous sinkholes, caverns, and underground streams. In contrast to the Mountain Pine Ridge, some of the soils in these regions are quite fertile and have been cultivated during at least the past 4,000 years.
Much of the northern half of Belize lies on the Yucatán Platform, a tectonically stable region. Although mostly level, this part of the country also has occasional areas of hilly, karst terrain, such as the Yalbac Hills along the western border with Guatemala and the Manatee Hills between Belize City and Dangriga. Alluvial deposits of varying fertility cover the relatively flat landscapes of the coastal plains.
Environmental degradation issues in Belize include deforestation, water pollution from sewage, industrial effluents, agricultural runoff, and solid waste disposal.
Belize is party to the Basel Convention, Convention on Biological Diversity, Ramsar Convention, CITES, Convention on the Prevention of Marine Pollution by Dumping of Wastes and Other Matter, International Convention for the Regulation of Whaling, Montreal Protocol, MARPOL 73/78, United Nations Convention on the Law of the Sea, United Nations Convention to Combat Desertification, and United Nations Framework Convention on Climate Change.
Although a number of economically important minerals exist in Belize, none has been found in quantities large enough to warrant their mining. Those minerals include dolomite, barite (source of barium), bauxite (source of aluminum), cassiterite (source of tin), and gold. In 1990 limestone, used in road building, was the only mineral resource being exploited for either domestic or export use.
The similarity of Belizean geology to that of oil-producing areas of Mexico and Guatemala prompted oil companies, principally from the United States, to explore for petroleum at both offshore and on-land sites in the early 1980s. Initial results were promising, but the pace of exploration slowed later in the decade, and production operations never commenced. As a result, Belize remains almost totally dependent on imported petroleum for its energy needs.
Belize has considerable potential for hydroelectric and other renewable energy resources, such as solar and biomass. In the mid-1980s a Belizean businessman proposed the construction of a wood-burning power station for the production of electricity, but the idea foundered in the wake of ecological concerns and economic constraints. In late 2005, a company named Belize Natural Energy found oil in commercial quantities in the Spanish Lookout area of Belize.
Belize, formerly British Honduras, is a country located on the north eastern coast of Central America. Belize is bordered on the northwest by Mexico, on the east by the Caribbean Sea, and on the south and west by Guatemala. It has an area of 22,970 square kilometres (8,867 sq mi) and a population of 408,487 (2019). Its mainland is about 180 mi (290 km) long and 68 mi (110 km) wide. It has the lowest population and population density in Central America. The country's population growth rate of 1.87% per year is the second highest in the region and one of the highest in the Western Hemisphere.
Costa Rica is located on the Central American Isthmus, surrounding the point 10° north of the equator and 84° west of the prime meridian. It borders both the Caribbean Sea and the North Pacific Ocean, with a total of 1,290 km of coastline.
El Salvador borders the North Pacific Ocean to the south and southwest, with Guatemala to the north-northwest and Honduras to the north-northeast. In the southeast, the Golfo de Fonseca separates it from Nicaragua. El Salvador is the smallest Central American country and is the only one without a coastline on the Caribbean sea.
Honduras is a country in Central America. Honduras borders the Caribbean Sea and the North Pacific Ocean. Guatemala lies to the west, Nicaragua south east and El Salvador to the south west. Honduras is the second largest Central American republic, with a total area of 112,890 square kilometres (43,590 sq mi).
Guatemala is mountainous, except for the south coastal area and the vast northern lowlands of Petén department. The country is located in Central America, bordering the Caribbean Sea, between Honduras and Belize and bordering the North Pacific Ocean, between El Salvador and Mexico. Two mountain chains enter Guatemala from west to east, dividing the country into three major regions: the highlands, where the mountains are located; the Pacific coast, south of the mountains; and the limestone plateau of the Petén region, north of the mountains. These areas vary in climate, elevation, and landscape, providing dramatic contrasts between hot and humid tropical lowlands and highland peaks and valleys.
The Riviera Maya is a tourism and resort district south of Cancun, Mexico. It straddles the coastal Federal Highway 307, along the Caribbean coastline of the state of Quintana Roo, located in the eastern portion of the Yucatán Peninsula. Historically, this district started at the city of Playa del Carmen and ended at the village of Tulum, although the towns of Puerto Morelos, situated to the north of Playa del Carmen, as well as the town of Felipe Carrillo Puerto, situated 40 kilometres (25 mi) to the south of Tulum, are both currently being promoted as part of the Riviera Maya tourist corridor.
The Yucatán Peninsula, in southeastern Mexico, separates the Caribbean Sea from the Gulf of Mexico, with the northern coastline on the Yucatán Channel. The peninsula lies east of the Isthmus of Tehuantepec, a northwestern geographic partition separating the region of Central America from the rest of North America. It is approximately 181,000 km2 (70,000 sq mi) in area, and is almost entirely composed of limestone.
The Mesoamerican Barrier Reef System (MBRS), also popularly known as the Great Mayan Reef or Great Maya Reef, is a marine region that stretches over 1,000 kilometres (620 mi) from Isla Contoy at the tip of the Yucatán Peninsula down to Belize, Guatemala and the Bay Islands of Honduras. The reef system includes various protected areas and parks including the Belize Barrier Reef, Arrecifes de Cozumel National Park, Hol Chan Marine Reserve (Belize), Sian Ka'an biosphere reserve, and the Cayos Cochinos Marine Park. Belize's coastline, including the Belize Barrier Reef, is home to approximately 80% of the Mesoamerican Barrier Reef System. The Belize Barrier Reef is the largest barrier reef in the northern hemisphere and the second largest barrier reef in the world. The Belize Barrier Reef and Belize's three offshore atolls, several hundred sand cays, mangrove forests, coastal lagoons and estuaries—collectively termed, the Belize Barrier Reef Reserve System—has been designated a World Heritage Site by UNESCO (1996).
The Sarstoon River is a river in the Toledo District of Belize. It forms the country's southern boundary with Guatemala.
The Sibun River is a river in Belize which drains a large central portion of the country. The Sibun (Xibun) where ancient Maya people who inhabited the region.
Monkey River is a coastal watercourse in southern Belize that rises in the Maya Mountains and discharges to the Caribbean Sea near Monkey River Town. One of Belize's major rivers, Monkey River has northern headwaters which originate in the Cockscomb Basin Wildlife Sanctuary, where the Swasey Branch drains the East Basin of that wildlife sanctuary. Further south, the Bladen Branch watercourse drains the eastern slopes of the Maya Mountains including the ancient Mayan settlement areas of Lubaantun and Nim Li Punit. These two watercourses join to form the Monkey River approximately 16 kilometres upstream from the mouth of the Monkey River. The Monkey River is readily navigated throughout the year using small boats, but navigation above the major confluence becomes more difficult due to lack of depth when the dry season starts about February. Habitats in this watershed provide cover for such diverse species as the ocelot, jaguar, Guatemalan black howler, bare-throated tiger heron, Morelet's crocodile, fer-de-lance and manatee.
The Petén-Veracruz moist forests ecoregion, of the Tropical and subtropical moist broadleaf forest Biome, is found in Belize, Guatemala, and Mexico.
This is an Index of Central America-related articles. This index defines Central America as the seven nations of Belize, Costa Rica, El Salvador, Guatemala, Honduras, Nicaragua, and Panama.
The following is an alphabetical list of topics related to the nation of Belize.
Hispanic Belizeans or Belizean Mestizos are Belizeans of Hispanic and mestizo descent. Currently, they comprise around 52.9% of Belize's population.
Sarstoon Island is an island at the southernmost point of Belize located near the mouth of the Sarstoon River. The Sarstoon River is located at the south of Sarstoon Island and is the southern part of the Belize–Guatemala border. Sarstoon Island is part of the Toledo District of Belize, which is one of 6 districts of the country. The island is mostly mangrove swampland and is uninhabited. It covers approximately 0.68 square kilometres (0.26 sq mi).
The 2016 Belize–Guatemala border standoff began when Belizean soldiers fatally shot a 13-year-old Guatemalan along the Sarstoon River, which marks Belize's southern border with Guatemala.
Belize–Spain relations are the bilateral and diplomatic relations between these two countries. Belize has an embassy and honorary consulates in Madrid, Barcelona and Palma de Mallorca. Spain has a non-resident embassy for Belize in Guatemala, and an honorary consulate in Belize City.
|Wikimedia Commons has media related to Geography of Belize .|