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2026/02/23

Brunei Darussalam Independence Day

Brunei, independent Islamic sultanate on the northern coast of the island of Borneo in Southeast Asia. It is bounded to the north by the South China Sea and on all other sides by the East Malaysian state of Sarawak, which also divides the state into two disconnected segments of unequal size. The western segment is the larger of the two and contains the capital city of Bandar Seri Begawan. Brunei achieved independence in 1984, having been a British protectorate since 1888. It is a member of the Commonwealth and ASEAN (Association of Southeast Asian Nations). Land - Relief, drainage, and soils Brunei consists of a narrow coastal plain in the north, which gives way to rugged hills in the south. The country’s highest point is Pagon Peak (6,070 feet [1,850 metres]), in the southeast. Brunei is drained by the Belait, Tutong, and Brunei rivers in the western segment and by the Pandaruan and Temburong rivers in the east; all flow generally northward to the South China Sea. The Belait is the largest river in the country. The soils of Brunei are deeply weathered, highly leached, and generally infertile. Richer alluvial soils are found along the rivers and in some parts of the coastal floodplain, and these offer the best agricultural potential. White quartz sands are prevalent in some areas. Climate The climate of Brunei is governed by the equatorial monsoon winds. The northeast monsoon typically blows from December to March, and the southwest monsoon blows from May to September. April, October, and November are transitional months. Temperatures in Brunei are warm throughout the year, typically dropping into the mid-70s F (about 23 °C) and rising to about 90 °F (32 °C) on a daily basis. Precipitation averages about 115 inches (2,900 mm) annually in the coastal areas but can exceed 150 inches (3,800 mm) farther inland. Rainfall is generally heavier from October to January and lighter from March to August. Plant and animal life About three-fifths of the country is covered with virgin tropical rainforest, and another one-fifth is under secondary forest. The undisturbed rainforest consists mainly of hardwoods of the Dipterocarpaceae family (notably of the genus Shorea), most of which are of commercial value. Large expanses of freshwater and peat swamps are found in the poorly drained lowlands of the Belait and Tutong rivers, while mangrove swamps are common along the lower riverine reaches and sheltered coastal areas. The complex vegetation of the rainforest provides niches for a rich variety of animals, including proboscis monkeys, leaf monkeys, pigtail macaques, gibbons, sun bears, sambar deer, pangolins, bats, and many other mammals. Among Brunei’s most notable birds are its argus pheasants and hornbills. Numerous species of reptiles, including the large reticulated python, inhabit the country’s swamps and woodlands. People - Ethnic groups Nearly two-thirds of the population of Brunei is classified officially as Malay. This category, however, includes not only ethnic Malays but also a number of the indigenous peoples, namely the Dusun, Belait, Kedayan, Murut, and Bisaya (Bisayah). Chinese make up about one-tenth of the population. The remainder of Brunei’s residents consists of other (non-Malay) indigenous peoples, such as the Iban (or Sea Dayak); various peoples of South Asian descent; and temporary workers, primarily from Asia and Europe. Languages The official language is Malay, with English as a major second language. Many Chinese speak southern varieties of Chinese, and many learn Mandarin in school. Religion Brunei’s population is predominantly Sunni Muslim, although the Chinese usually follow Buddhism, Daoism, Confucianism, or Christianity. Some of the indigenous peoples are Christian, while others follow their own local religions. Settlement patterns The forested uplands of Brunei’s interior are sparsely populated by indigenous peoples, who practice shifting agriculture. In the country’s western segment, the Iban and the Belait generally inhabit the westernmost region near the border with Sarawak, while the Kedayan are concentrated in the central and eastern areas, and the Kadazan live primarily in the rural parts of the east-central region. The Murut and Bisaya have settled mainly in the eastern segment of Brunei. The Malays are distributed in the riverine and coastal villages and towns throughout the country, and the Chinese are concentrated in the urban areas. About two-thirds of Brunei’s population is found in and around Bandar Seri Begawan, the capital and largest urban centre. The city is located on the Brunei River about 9 miles (14 km) from its mouth on Brunei Bay. Adjacent to the modern section of the city is an older part called Kampong Ayer, where Brunei Malays live in houses built on stilts along inlets of the river. The area surrounding the cities of Kuala Belait and Seria, both in the oil-rich zone of the southwestern coast, is the country’s next most densely settled region. Demographic trends The population of Brunei is youthful and growing. More than one-fifth of the population is under age 15, and roughly half is under age 30. The birth rate is around the global average, while the death rate is among the lowest in the world, partly because of the youthful age distribution. Life expectancy is around 78 years of age, higher than the global average. Brunei has a high net migration rate, though its growth rate is steadily decreasing. Economy of Brunei Brunei’s economy is almost totally dependent on the exploitation of its vast reserves of petroleum and natural gas. Although oil and gas revenues have allowed the state to give its citizens one of the highest per capita incomes in Asia, they also have made the country dependent on a single commodity that is subject to market fluctuations. In addition, Brunei must rely on imports for nearly all its manufactured goods and most of its food. In an effort to ensure the country’s economic stability, the government has since the late 20th century striven to diversify the economy by developing other sectors, such as agriculture, fisheries, tourism, and financial services. Agriculture, fishing, and forestry Agriculture, fishing, and forestry, once the mainstays of Brunei’s economy, declined in importance after the discovery of petroleum resources in the 1920s. By the end of the 20th century, these three activities accounted for just a tiny fraction of the gross domestic product (GDP) and employed a comparably small segment of the workforce. Recognizing a need to diversify the economy away from petroleum production as well as to reduce the country’s dependence on food imports, the government subsequently embarked on a program to develop the agricultural industry. By the early 21st century Brunei had become self-sufficient in the production of poultry and eggs and was approaching self-sufficiency in vegetables. Although locally grown rice still fell far short of domestic need, production had increased markedly. Brunei is among the largest consumers of fish per capita in the world. Fish imports reached a high in the mid-1990s. In an effort to curb imports, the government implemented programs to stimulate local fisheries. Within a decade Brunei was producing more fish domestically than it imported. Overfishing has been a growing concern, however, despite the government’s emphasis on sustainable development. Aquaculture has been encouraged in carefully selected areas. With an aim of preserving the country’s abundant forest cover, Brunei enacted legislation in the late 20th century to restrict logging. Plantation programs have been implemented to provide enough sawed wood for the local market only. Timber is not exported. Resources and power The petroleum industry (including the manufacture of liquefied natural gas [LNG]) generates more than half of Brunei’s GDP, although it employs a very small portion of the labour force. Nearly all of the country’s petroleum and natural gas is produced from offshore fields located off its own western segment, and all but a small percentage of the production is exported, mostly to Asian countries. A local refinery supplies domestic needs; the country’s energy is generated almost entirely from fossil fuels. Oil was first produced in 1929, while the natural gas industry was developed after the discovery in the 1960s of large deposits. Output of oil reached a peak in the late 1970s and subsequently was reduced in order to conserve reserves. Intensive exploitation of the country’s huge deposits of natural gas in the 1970s included the construction of a liquefaction plant, and LNG has since become a major source of Brunei’s export earnings. In addition to its hydrocarbon reserves, the country has rich deposits of white quartz sand that remained virtually undeveloped in the early 21st century. Finance and trade In lieu of a central bank, the Financial Institution Division and the Brunei Currency Board, both part of the Ministry of Finance, are responsible for most central banking services. The Brunei Currency Board issues the Brunei dollar. Several Islamic commercial banks, a number of foreign banks, and a few offshore banks all operate in the country. Much of the state’s financial activity is concerned with managing its substantial foreign investments, and the return on these has become an important source of income. Revenues from petroleum and natural gas, which constitute nearly all of the country’s export earnings, have generally resulted in trade surpluses since the early 1970s. The country’s principal trading partners are in Asia and include Japan, Singapore, Malaysia, China, South Korea, and India. Brunei also trades with the United States, Australia, New Zealand, and members of the European Union to varying degrees. Brunei has been a member of ASEAN since 1984 and became home to the secretariat of the East ASEAN Business Council in the mid-1990s. More … Source: https://www.britannica.com/place/Brunei

2026/02/23

Republic Day of the Cooperative Republic of Guyana

Guyana, country located in the northeastern corner of South America. Indigenous peoples inhabited Guyana prior to European settlement, and their name for the land, guiana (“land of water”), gave the country its name. Present-day Guyana reflects its British and Dutch colonial past and its reactions to that past. It is the only English-speaking country of South America. Since Guyana gained its independence in 1966, the country’s chief economic assets have been its natural resources, mainly its pristine rainforests, sugarcane plantations, rice fields, and bauxite and gold reserves. Despite those riches, Guyana remained one of the poorest countries in South America into the first decades of the 21st century, but the country’s economic fortunes changed dramatically in 2015 with the first of a raft of rich deepwater oil field discoveries in Guyana’s offshore Stabroek Block. Some geographers classify Guyana as a part of the Caribbean region, which they deem to include the West Indies as well as Guyana, Belize, Suriname, and French Guiana on the South American mainland. The capital and chief port of Guyana is Georgetown. Guyana’s populace is mainly of colonial origin, although Indians are scattered throughout the forested interior. The more numerous coastal peoples are chiefly descendants of slaves from Africa and indentured workers from India, who were originally transported to work the coastal sugarcane plantations. Ethnic problems between the last two groups have played a disruptive role in Guyanese society. Guyana has been a member of the Commonwealth (an international group made up of the United Kingdom and a number of its former dependencies) since 1970. Politically, however, Guyana moved on a steady course toward communism from the time of independence until the death of the first prime minister, Forbes Burnham, in 1985, after which ties with Western powers were strengthened, and by the 1990s privatization had begun. Land Guyana is bordered by the Atlantic Ocean to the north, by Suriname (along the Courantyne River) to the east, by Brazil to the south and southwest, and by Venezuela to the west. Guyana is involved in territorial disputes with both Suriname and Venezuela that are legacies of colonial rule. Although a United Nations international tribunal settled a long-standing maritime boundary dispute between Guyana and Suriname in 2007, the latter still claims the New River Triangle, a 6,000-square-mile (15,600-square-km) area between two tributaries of the Courantyne River in southern Guyana. The currently recognized border between Suriname and Guyana along the Courantyne is also in contention—Suriname claims sovereignty over the entire river and thus views its west bank as the border, while Guyana claims that the thalweg, or deepest channel of the river, is the boundary. The dispute between Guyana and Venezuela dates from 1895, when the British government claimed ownership of the Essequibo River basin. An 1899 settlement awarded Venezuela part of the area, but in 1962 Venezuela claimed all the territory west of the Essequibo. Relief The narrow plain that extends along the country’s Atlantic coast has been modified considerably by humans. Much of the area, which measures only about 10 miles (16 km) at its widest point, has been reclaimed from the sea by a series of canals and some 140 miles (225 km) of dikes. The coastal plain’s inland border is generally marked by canals that separate the plain from interior swamps. About 40 miles (65 km) inland from the coast is a region of undulating land that rises from 50-foot (15-metre) hills on the eastern, coastal side of the region to 400-foot (120-metre) ones on the western side. The area is between 80 and 100 miles (130 and 160 km) wide and is widest in the southeast. It is covered with sand, from which it takes its name as the white-sands (Zanderij) region. A small savanna region in the east lies about 60 miles (100 km) from the coast and is surrounded by the white-sands belt. The sand partly overlies a low crystalline plateau that is generally less than 500 feet (150 metres) in elevation. The plateau forms most of the country’s centre and is penetrated by igneous rock intrusions that cause the numerous rapids of Guyana’s rivers. Beyond the crystalline plateau, the Kaieteurian Plateau lies generally below 1,600 feet (490 metres) above sea level; it is the site of the spectacular Kaieteur Falls, noted for their sheer 741-foot (226-metre) initial plunge. The plateau is overlain with sandstones and shales that in the south form the extensive Rupununi Savanna region. The Acaraí Mountains, which rise to about 2,000 feet (600 metres), rim the plateau on the southern border, and it is crowned on the western frontier by the Pakaraima Mountains, which rise to 9,094 feet (2,772 metres) at Mount Roraima. The Rupununi Savanna is bisected by the east–west-trending Kanuku Mountains. Guyana’s four main rivers—the Courantyne, Berbice, Demerara, and Essequibo—all flow from the south and empty into the Atlantic along the eastern section of the coast. Among the tributaries of the Essequibo, the Potaro, the Mazaruni, and the Cuyuni drain the northwest, and the Rupununi drains the southern savanna. The coast is cut by shorter rivers, including the Pomeroon, the Mahaica, the Mahaicony, and the Abary. The rivers are part of the watershed of the Amazon and Orinoco rivers, and the headwaters of the Rupununi in Brazil are often confused with those of the Amazon. Drainage is poor because the average gradient is only about 1 foot per mile (19 centimetres per km), and there are swamps and flooding in the mountains and savannas. The rivers are not suitable for long-distance transportation because they are broken by interior falls, and in the coastal zone their mouths and estuaries are blocked by mud and by sandbars that may occur 2 to 3 miles (about 4 km) out to sea. Soils The coastal soils are fertile but acidic. The fine-particle grayish blue clays of the coastal plain are composed of alluvium from the Amazon (the mouth of which lies east of Guyana, on the Brazilian coast) deposited by the south equatorial ocean current and of much smaller amounts of alluvium from the country’s rivers. They overlie white sands and clays and can support intensive agriculture but must be subjected to fallowing to restore fertility. Pegasse soil, a type of tropical peat, occurs behind the coastal clays and along the river estuaries, while silts line the banks of the lower rivers. Reef sands occur in bands in the coastal plain, especially near the Courantyne and Essequibo rivers. The rock soils of the interior are leached and infertile, and the white sands are almost pure quartz. Climate of Guyana High temperatures, heavy rainfall with small seasonal differences, high humidity, and high average cloud cover provide climatic characteristics of an equatorial lowland. Temperatures are remarkably uniform. At Georgetown the daily temperature varies from the mid-70s to the mid-80s °F (mid-20s to the upper 20s °C). The constant heat and high humidity are mitigated near the coast by the trade winds. Rainfall derives mainly from the movement of the intertropical front, or doldrums. It is heavy everywhere on the plateau and the coast. The annual average at Georgetown is about 90 inches (2,290 mm), and on the interior Rupununi Savanna it is about 70 inches (1,800 mm). On the coast a long wet season, from April to August, and a short wet season, from December to early February, are sufficiently well marked on the average, but in the southern savannas the short wet season does not occur. Total annual rainfall is variable, and seasonal drought can occur in July and August when the southeast trade winds parallel the coast. Variations in Guyana’s climatic patterns have a determining effect on tropical crop production. Plant and animal life Many plants of the coast, including mangroves and various saltwater grasses, grow in shallow brackish water and help to protect or extend the land. The wet savanna behind the coast has coarse tufted grasses and a wide scattering of palms, notably the coconut, the truli, and the manicole. High rainforest, or selva, covers about three-fourths of the land area and is of extraordinary variety and magnificence. Prominent trees include the greenheart and the wallaba on the sandy soils of the northern edge, the giant mora and the crabwood on swampy sites, the balata and other latex producers, and many species such as the siruaballi and the hubaballi that yield handsome cabinet woods. The interior savanna is mostly open grassland, with much bare rock, many termite hills, and clumps of ita palm. All forms of animal life are immensely varied and abundant, though few, apart from birds and insects, are normally visible. The tapir is the country’s largest land mammal, and the jaguar is the largest and fiercest of the cats, which also include the ocelot; monkeys and deer are the most common animals. Among the more exotic species are the sloth, the great anteater, the capybara (bush pig), and the armadillo. Birds include the vulture, the kiskadee, the blue sacki, the hummingbird, the kingfisher, and the scarlet ibis of the coast and lower rivers and the macaw, the tinamou, the bell-bird, and the cock-of-the-rock in the forest and savanna. The caiman (a reptile similar to the alligator) is the most common of the larger freshwater creatures. The giant anaconda, or water boa, is the largest of the many kinds of snakes, and the bushmaster is the most vicious. Lizards are numerous and include the iguana in the lower rivers. Sharks and stingrays are found offshore. The snapper and the grouper are common ocean fish, and shrimp abounds in the muddy currents off the coast. The manatee is also common in Guyanese waters. Among the freshwater fish is the huge piraucu, which attains lengths up to 14 feet (430 cm). More … Source: https://www.britannica.com/place/Guyana  

2026/02/23

Independence day of Saint Lucia

Saint Lucia, island state in the Caribbean Sea. It is the second largest of the Windward group in the Lesser Antilles and is located about 24 miles (39 km) south of Martinique and some 21 miles (34 km) northeast of Saint Vincent. Saint Lucia is 27 miles (43 km) long and has a maximum width of 14 miles (23 km). The capital and major port is Castries. Saint Lucia is a member of the Commonwealth. Land - Relief and drainage The island is of volcanic origin and is bisected from north to south by a central ridge of wooded mountains, the highest point being Mount Gimie (3,145 feet [959 metres]). Many streams flow from the mountains through fertile valleys. In the southwest are the Gros and Petit Pitons (2,619 feet [798 metres] and 2,460 feet [750 metres], respectively), two immense pyramids of rock rising sharply from the sea and enclosing a small bay. Near Petit Piton, in the crater of an ancient volcano, are the boiling sulphur springs from which the nearby town of Soufrière takes its name. A choice tourist site, the springs also contain substantial energy potential. Climate Saint Lucia lies in the path of the northeastern trade winds and has a tropical maritime climate. Rainfall and temperature vary with elevation. Average annual rainfall ranges from 51 inches (1,295 mm) on the coast to as much as 150 inches (3,810 mm) in the interior. There is a dry season roughly from January to April and a rainy season from May to November. The mean temperature is about 80 °F (27 °C), with highs sometimes ranging into the upper 80s (31 °C) and lows into the upper 60s (20 °C). Plant and animal life The forest, which has been reduced through lumbering, contains colourful orchids and anthurium. The rich birdlife includes the Saint Lucian parrot (the endangered national bird), the Saint Lucia black finch, and the Saint Lucia oriole. There is also a lizard unique to Saint Lucia, and the agouti is common. People No Caribs remain on the island; the vast majority of the inhabitants of the island are black and there is a small minority of mulattoes and other mixtures. The remainder are whites or of East Indian extraction. A French patois is spoken by most of the inhabitants but is being gradually supplanted by English, the official language. The main religion is Roman Catholicism, and Seventh-day Adventists and other Protestants are important minorities. The rate of population growth for Saint Lucia is slightly higher than the Caribbean average. The main population centres are Castries and Vieux Fort. Economy - Agriculture, forestry, and fishing Sugarcane was formerly the chief crop, but production ceased entirely in 1964, when most of the cane fields were converted to banana cultivation. Bananas are now the principal crop. Other crops are coconuts, cacao, citrus and other fruit, spices, cassava, and yams. There is a steady local fishing industry. Manufacturing Saint Lucia’s manufacturing sector has been a major beneficiary of the U.S. Caribbean Basin Initiative, a program designed to promote manufacturing in the region. An industrial free zone has been established in the south of the island near Vieux Fort; there factories produce and export electronic goods and toys. Other industries produce cardboard cartons, clothing, rum, tobacco products, coconut products, concrete blocks, and beer. Tourism has developed rapidly since 1970; in 1987 a complex for cruise ships was opened near Castries. Trade The chief exports are bananas, cardboard cartons, clothing, coconut products, and electronic goods. Saint Lucia’s major trading partners are the United States, Trinidad and Tobago, the United Kingdom, Barbados, and Dominica. Imports include food, fuels, and manufactured goods. Transportation There is an international airport at Vieux Fort, at the southern tip of the island, and a smaller airport at Vigie for domestic and regional flights. International shipping lines operate from the ports at Castries and Vieux Fort. In addition, there is an oil transshipment terminal near Castries. Government and society - Constitutional framework Saint Lucia is a constitutional monarchy with the British monarch as head of state, represented by a governor-general. The bicameral parliament consists of the House of Assembly elected by universal adult suffrage and the Senate, with members appointed on the advice of the prime minister, on the advice of the opposition leader in the House, and by the governor-general. The prime minister, leader of the majority party, heads the government. Justice Saint Lucia has retained its association with the Eastern Caribbean Supreme Court, consisting of a court of appeal and a high court. Health and welfare Several general hospitals and many health centres are distributed throughout the island. There is also a private hospital operated by a religious order at Vieux Fort. Education Primary education is free and compulsory, and there is a branch of the University of the West Indies at Castries. There is also a technical college and a teacher-training college. Many of the primary schools are parochial, principally Roman Catholic. Communications Several newspapers are published on the island, and radio and television broadcasts are widely received. History of Saint Lucia - French and British territorial rivalry The exact date of the European discovery of Saint Lucia is not known, but it is thought to have been about 1500. The first attempts at colonization were made by the English in 1605 and 1638, but they were frustrated by sickness and the hostility of the native Caribs. A successful settlement was achieved in 1650 by the French from Martinique, who made a treaty with the Caribs in 1660. In 1664 Thomas Warner, son of the governor of Saint Kitts, regained the island, but it was restored to France by the Treaty of Breda in 1667. In 1674 it was claimed by the crown of France and made a dependency of Martinique. Another British settlement under a grant made in 1722 by George I to the duke of Montague was frustrated by France, which had granted the island to Marshal d’Estrées in 1718, and the island was declared neutral. In 1743 the French resumed possession, retaining the island until the Treaty of Aix-la-Chapelle in 1748, in which the two countries again agreed to regard Saint Lucia as neutral. In 1762 it was captured by Adm. George Rodney and Gen. Robert Monckton, only to be given up once more by the Treaty of Paris (1763). In 1778 it again surrendered to the British, who used its harbours as a naval base, but, by the Peace of Versailles, Saint Lucia was once more restored to France. Between 1782 and 1803 the possession of Saint Lucia passed several times between Britain and France, the British having to suppress a vigorous revolutionary party, which was aided by insurgent slaves, before gaining possession in 1803. Saint Lucia was finally ceded to Britain in 1814 by the Treaty of Paris, after which it became a crown colony. During 1838–85, together with the other islands of the Windward group, it was administered by the governor of Barbados. French influence on the development of Saint Lucia is illustrated by the dominance of the Roman Catholic Church and the survival of a French patois. In the years following 1763, French planters came from Saint Vincent and Grenada and established cotton and sugar plantations. In 1834, when the slaves were emancipated, there were in Saint Lucia more than 13,000 black slaves, 2,600 free blacks, and 2,300 whites. Prosperity was impeded by the decline of the sugarcane industry. Improvement came with the increase of banana and cacao cultivation and the revival of sugarcane. More … Source: https://www.britannica.com/place/Saint-Lucia    

2026/02/22

Brunei (Asia) Vacation Travel Video Guide

Travel video about destination Brunei.

2026/02/22

Welcome to Guyana

When it is safe to travel again, we'll be here waiting for you, waiting to say: Welcome back to nature. Welcome to Guyana. #DiscoverGuyana #HappyEarthDay

2026/02/22

St. Lucia City Video Guide | Expedia

St. Lucia City Video Guide

2026/02/21

Holiday | Tourism Information | Visit The Gambia | Gambia

In The Gambia, we boast of diverse cultures, history, and an abundance of sandy beaches. From unforgettable boat rides on the River Gambia to natural ...

2026/02/20

Independence day of the Republic of Gambia

The Gambia, country in western Africa situated on the Atlantic coast and surrounded by the neighbouring country of Senegal. It occupies a long narrow strip of land that surrounds the Gambia River. The land is flat and is dominated by the river, which is navigable throughout the length of the country. The peculiar shape and size of the country are the result of territorial compromises made during the 19th century by Great Britain, which controlled the lower Gambia River, and France, which ruled the neighbouring colony of Senegal. Periodic talks in the 20th century to unite The Gambia and Senegal led to the short-lived Senegambia confederation (1982–89). The Gambia is Africa’s smallest nonisland country. It is also one of Africa’s most densely populated countries. A few towns are located upriver, but most Gambians live in rural villages. The major ethnic groups are similar to those in Senegal and consist of the majority Malinke and also include Wolof, Fulani (Fulbe), Diola (Jola), and Soninke peoples. The Gambian economy is heavily dependent on peanut (groundnut) production and export. The country is known for the beaches along its small Atlantic coastline and for being home to Jufureh (Juffure), the reputed ancestral village of Kunta Kinte, the main character in Alex Haley’s well-known novel Roots. The capital, Banjul (called Bathurst until 1973), is situated where the Gambia River flows into the Atlantic Ocean. Land The Gambia is a strip of land 15 to 30 miles (25 to 50 km) wide on either side of the Gambia River and extends almost 300 miles (480 km) into the interior; except for a short coastline along the Atlantic Ocean, it is entirely surrounded by Senegal. Relief and drainage The Gambia River is the country’s dominant feature. It flows across a plateau of Miocene-Pliocene sandstone consisting of compacted sediment composed predominantly of quartz grains formed from about 23.7 to 1.6 million years ago. In the east, narrow valleys are separated by broad interfluves or flattish hills. In the west, lower and smaller sand hills alternate with depressions filled in with sand to form a flat plain. Soils and climate The Gambia has a wet-and-dry tropical climate characterized by an intense rainy season occurring generally between June and October and by a longer dry season. Near the coast the rainy season lasts longer, and the rainfall is heavier, diminishing eastward. At Yundum the average annual rainfall is about 50 inches (1,300 mm), and the mean monthly temperature tends to be in the upper 70s F (mid-20s C), while at Basse Santa Su, about 270 miles (435 km) inland, the comparable figures are about 40 inches (1,000 mm) and the low 80s F (upper 20s C). The relative humidity is high but drops from December to April, when the dry northeastern wind known as the harmattan is dominant. Plant and animal life The vegetation cover of The Gambia is savanna on the uplands, various kinds of inland swamp in the low-lying areas, and mangrove swamp along the brackish lower Gambia River. Few wild animals are native to the region, and those that survive are under pressure from the human and domestic animal populations. In the middle and upper river areas there are warthogs, monkeys, baboons, antelope, pygmy hippopotamuses, and crocodiles. In addition, more than 500 species of birds live throughout the country. Birds and wildlife can be found in Bijilo Forest Park, along the Atlantic coast, the Abuko Nature Reserve, just upriver from Banjul, Kiang West National Park, farther inland, and River Gambia National Park (also known as Baboon Island National Park), near Kuntaur. People - Ethnic groups The river basin was a focal point for migrating groups of people escaping the turmoil of western Sudanic wars dating from the 12th century. The Diola (Jola) are the people longest resident in the country; they are now located mostly in western Gambia. The largest group is the Malinke, comprising about one-third of the population. The Wolof, who are the dominant group in Senegal, also predominate in Banjul. The Fulani settled the extreme upriver areas, and their kingdom, Fuladu, became a major power in the late 19th century. The Soninke, an admixture of Malinke and Fulani, are also concentrated in the upriver areas. Languages English is the official language, but the most frequently spoken languages are generally of the Atlantic branch of the Niger-Congo family. Mandinka and Wolof constitute the lingua francas of the country, and other languages spoken include Pulaar (Fulbe), Serer, Diola, and Soninke. Some Muslim clerics are literate in Arabic. Religion The population is overwhelmingly Muslim. There are a small number of Christians—predominantly Roman Catholic—and some adherents of traditional beliefs. Settlement patterns Human settlement in The Gambia extends across both banks of the river and is found in three regions: the swamps adjacent to the river, the riverine flats, known as banto faros (from a Mande word meaning “beyond the swamp”), and the sandstone uplands. Most rural settlement is concentrated on the uplands, which have the best-drained soils. A number of settlements are located in the banto faros on the middle course of the river, where there is less danger of flooding than in the swamps. Many villages are built on the boundary between the uplands and the riverine flats. About three-fifths of the population lives in urban areas. The major urban concentration is around Banjul, the capital, and several large urban centres have developed in the vicinity. Urban dwellers retain close ties to their rural relatives, and there is considerable interaction between rural and urban populations. Migration to urban areas has remained steady since the 1970s. Demographic trends The population growth rate and infant mortality rate in The Gambia are among the highest in western Africa. The population is young, with about two-thirds under age 30. Life expectancy is comparable to the regional average but lower than that of the world. Over the years, conflict in other western African countries led to an influx of refugees into The Gambia, most notably those fleeing from fighting in Senegal’s Casamance region as well as those who fled from civil wars in Liberia and Sierra Leone. Economy - Agriculture, forestry, and fishing Gambian agriculture can be described as a classic monoculture; peanuts (groundnuts) are the most valuable agricultural commodity. Land is cleared by the slash-and-burn technique, but farmers practice conservation. Most land is held in common by the villagers. There is a sharp division of labour, with men involved in planting, cultivating, and harvesting cash crops while women cultivate subsistence crops such as cassava (manioc), yams, eggplant, tomatoes, rice, and lentils. There are citrus orchards in the western area near Banjul. The production of peanuts has increased with the wider use of fertilizers and ox-drawn equipment and the introduction of better seeds. In order to diversify the economy, the government has encouraged the production of rice. A pilot scheme was begun in the mid-1960s to introduce plantation oil palm production, but this has had little impact on the national economy. Stock farming, always a factor in the Fulani culture, has also received government support, but factors such as insufficient animal husbandry techniques and the scarcity of suitable pasture and water have limited the size of herds. The drought years of the 1970s and ’80s seriously damaged agricultural production, particularly upriver. The country was not as hard hit as other countries in the region, however, and recovery has been steady. Although the country’s small ocean coastline limits marine fishing, there is some potential for commercial fishing offshore and in the river. Most Gambians are not fishermen, but those who are have been handicapped by inadequate equipment. The government has offered small loans for the purchase of motorized fishing boats and the construction of smoke huts for the processing of bonga (shad, or West African herring), which is exported to other western African states. Resources and power The Gambia has very few exploited mineral deposits. Some amounts of clay, sand, and gravel are excavated for local use. Foreign investors have been granted licenses to explore offshore blocks for potential petroleum and natural gas reserves, but these actions have not yet yielded any production. The Gambia River holds hydroelectric potential, but there are no dams on the river within the country’s borders. Oil is imported to meet the country’s energy needs. Electricity is limited to parts of Banjul and a few interior towns but is sporadic at best; most Gambians do not have access to modern infrastructure. Manufacturing The most significant industry in the country is peanut processing. The crop is sold to agents of The Gambia Groundnut Corporation (until 1993 known as the Gambia Produce Marketing Board), which fixes the season’s price in advance, pays the producers in cash, and sells the crop overseas. The agents arrange for transportation of the peanuts to Banjul or Kuntaur, where the nuts are shelled before being shipped. After shelling, a large part of the crop is pressed into oil at pressing mills. The residue is used as cattle cake. The construction industry has grown in correlation with the growth of the tourism sector. Smaller industries include the manufacture of food products, beverages, textiles, footwear, and wood products. Handicraft and other small-scale local craft production exists in villages throughout the country. More … Source: https://www.britannica.com/place/The-Gambia  

2026/02/18