Independence Day of the Commonwealth of the Bahamas

The Bahamas, archipelago and country on the northwestern edge of the West Indies. Formerly a British colony, The Bahamas became an independent country within the Commonwealth in 1973. The name Bahamas is of Lucayan Taino (Arawakan) derivation, although some historians believe it is from the Spanish bajamar, meaning “shallow water.” The islands occupy a position commanding the gateway to the Gulf of Mexico, the Caribbean Sea, and the entire Central American region. Their strategic location has given the history of The Bahamas a unique and often striking character. It was there that Christopher Columbus made his original landfall in the Americas. The subsequent fate of the peaceful original inhabitants remains one of the more tragic episodes in the development of the entire region, while the early attempts at European-dominated settlement were marked by intense national rivalries, interspersed with long periods of lawlessness and piracy. As a result, the society and culture that has evolved in The Bahamas is a distinctive blend of European and African heritages, the latter a legacy of the slave trade and the introduction of the plantation system using African slaves. The islands, lacking natural resources other than their agreeable climate and picturesque beaches, have become heavily dependent on the income generated by the extensive tourist facilities and the financial sector that have been developed, often as a result of the injection of foreign capital. The continued popularity of the islands with tourists, largely from North America, has helped to maintain a relatively high standard of living among the population, most of whom are of African descent. The capital, Nassau, is located on small but important New Providence Island. Land Lying to the north of Cuba and Hispaniola, the archipelago comprises nearly 700 islands and cays, only about 30 of which are inhabited, and more than 2,000 low, barren rock formations. It stretches more than 500 miles (800 km) southeast-northwest between Grand Bahama Island, which has an area of 530 square miles (1,373 square km) and lies about 60 miles (100 km) off the southeastern coast of the U.S. state of Florida, and Great Inagua Island, some 50 miles (80 km) from the eastern tip of Cuba. The islands other than New Providence are known collectively as the Out (Family) Islands. They include Grand Bahama, which contains the major settlements of Freeport and West End; Andros (2,300 square miles [6,000 square km]), the largest island of The Bahamas; Abaco, or Great Abaco, (372 square miles [963 square km]); and Eleuthera (187 square miles [484 square km]), the site of one of the early attempts at colonization. Relief and soils The Bahamas occupies an irregular submarine tableland that rises out of the depths of the Atlantic Ocean and is separated from nearby lands to the south and west by deepwater channels. Extensive areas of flatland, generally a few feet in elevation, are the dominant topographic features of the major islands; the Bimini group (9 square miles [23 square km]), for example, has a maximum elevation of only 20 feet (6 metres). A number of islands fronting the Atlantic have a range or series of ranges of hills on the northeastern side that parallel the longer axes of the islands. These ranges are formed of sand washed ashore and blown inland by the trade winds. The newer hills adjacent to the seashore are normally sand dunes. Solidity increases toward the interior, where the particles become cemented to form Bahama limestone. Eleuthera and Long Island (230 square miles [596 square km]) have the greatest number of hills exceeding 100 feet (30 metres). The highest point in The Bahamas, Mount Alvernia, at 206 feet (63 metres), is on Cat Island (150 square miles [388 square km]). Beneath the soil, the islands are composed of limestone rock and skeletal remains of coral fossils and other marine organisms. There are no rivers, but several islands—particularly New Providence, San Salvador (63 square miles [163 square km]), and Great Inagua—have large lakes. There is abundant fresh water on Andros Island. Climate of the The Bahamas The Bahamian climate, mild throughout the year, is one of the great attractions of the area. The average temperature varies from the low 70s F (about 21 °C) during the winter to the low 80s F (about 27 °C) during the summer, and extremes seldom fall below the low 60s F (about 16 °C) or rise above the low 90s F (about 32 °C). The average annual rainfall is about 44 inches (1,120 mm), occurring mostly during the summer months. Prevailing winds, coming from the northeast in winter and from the southeast in summer, lend a cooling influence to a generally humid atmosphere. Tropical cyclones (hurricanes) pose a threat during the period from June to November and have occasionally caused great destruction. Plant and animal life Extensive and beautiful forests of Caribbean pine are found on Grand Bahama, Abaco, Andros, and New Providence islands. Hardwood forests also occur on some of the islands. Elsewhere the woody vegetation consists mostly of shrubs and low trees. Animal life is dominated by frogs, lizards, and snakes, all of them nonpoisonous, and several species of bats are found in caves along the more rocky coasts. Larger animals include the agouti, a rodent; the raccoon; the iguana; and the elegant flamingo, the national bird. All of these have been much reduced in numbers and in distribution. In addition, several animals—notably sheep, horses, and other livestock—have been introduced from Europe. The surrounding waters abound with fish and other edible marine animals, such as conch and spiny lobster (crayfish). More … Score: https://www.britannica.com/place/The-Bahamas  

2025/07/10

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2025/07/07

Independence Day Union of the Comoros

Comoros, an independent state comprising three of the Comoro Islands in the Indian Ocean, off the coast of East Africa. A fourth island of the Comorian archipelago, Mayotte, is claimed by the country of Comoros but administered by France. The volcanic islands of the Comorian archipelago have been called the “perfumed islands” for their fragrant plant life and are known for their great scenic beauty. The four main islands of the archipelago—“four small effervescent stones, wedged between the nearby large red island [Madagascar] and the Mozambican coast,” in the words of the Comorian writer Sitti Saïd Youssouf—combine African, Arabic, Malagasy, and French influences and were once important in the significant Indian Ocean trade between East Africa and Asian ports such as India and Japan. Although the early history of the islands is uncertain, they are thought to have been explored by Arab and Persian traders in antiquity and, like Madagascar, settled by small numbers of Malayo-Indonesian peoples, gaining a sizable population only when Bantu-speaking peoples from the African mainland settled there. Shīrāzi Persians are thought to have arrived later, establishing Sunni Islam as the dominant religion. The ensuing Shīrāzi sultanates established trade relations with other countries along the Indian Ocean and developed a thriving economy based on the sale of spices and slaves. The opening of the Suez Canal substantially lessened the islands’ importance as an entrepôt, though not their strategic value. European colonial powers agreed that the Comorian archipelago would come under French rule in 1886–87, and it became an overseas territory of France in 1947. Three of the islands gained independence in 1975.Comoros is poor, witnessing an ongoing exodus of educated and skilled workers to France and a steady decline in gross domestic product. The capital, Moroni, located on the island of Grande Comore (N’gazidja), has most of the modern commercial and manufacturing facilities located in the country; in the absence of other possibilities, most islanders must rely on subsistence farming. With miles of beautiful beaches, tourists have always been drawn to Comoros. The islands’ history of political unrest, however, has hampered efforts to promote tourism. Land The Comoros are a group of islands at the northern end of the Mozambique Channel of the Indian Ocean, between Madagascar and the southeast African mainland, about 180 miles (290 km) off the eastern coast of Africa. The islands from northwest to southeast include Grande Comore (N’gazidja), Mohéli (Mwali), Anjouan (Ndzuwani), and Mayotte (Mahore). Relief, drainage, and soils The islands emerged from the floor of the Indian Ocean as a result of volcanic activity. Coral reefs provide occasional barriers to the rolling seas of the Indian Ocean, and breakers mark some of the world’s best diving areas. Along the seashore, broad expanses of open sandy beaches are interrupted by isolated groups of coconut palms or mangrove trees. A few coastal areas are distinguished by the harsh dark tangle of recent lava flows, while others are covered by smoothly rounded rocks, eroded reminders of ancient volcanic activity. Grande Comore is the largest and loftiest island. It rises near its southern end in an active volcano, Mount Karthala, which, at 7,746 feet (2,361 metres), is the country’s highest point. Karthala has erupted more than a dozen times in the past two centuries. The capital, Moroni, lies in the shadow of the volcano along the island’s west coast; the town of Mitsamiouli lies on the north coast. North of Mount Karthala is a wide plateau averaging 2,000 feet (600 metres) in elevation. The surface is generally rocky and the soils shallow. There are no perennial streams, and the coast, without large inlets, is ill suited for shipping. Mohéli is the smallest island of the group. Composed largely of a plateau that averages about 1,000 feet (300 metres) in elevation, the island ends in the west in a ridge reaching more than 2,600 feet (790 metres) above sea level. The valleys are generally fertile, and the hillsides are covered with thick forests. A strong sea swell hampers shipping. Mohéli’s chief towns are Fomboni on the northern coast and Nioumachoua in the southwest. Anjouan is a triangular island rising centrally in a volcanic massif (Mount Ntingui) that reaches an elevation of about 5,200 feet (1,580 metres). Although the soil cover is good, much erosion has occurred, and many areas are no longer arable. There are no good natural harbours. Moutsamoudou, on the northwest coast, is the chief town; its port facilities were modernized in the mid-1980s. Southeast of Anjouan lies Mayotte, the oldest of the four islands. It is claimed by Comoros (a claim recognized by the United Nations General Assembly), but its status is unsettled, and it continues to be administered by France. Climate The tropical climate has two clearly marked seasons: a cooler, dry period between May and October and a warmer, humid season between November and April. In November the summer monsoon (kashkazi) brings the highest afternoon temperatures—about 91 °F (33 °C). The highest monthly rainfall occurs in January with about 11–15 inches (275–375 mm), and the rainy season is the season of greatest tropical cyclone frequency. Dry season daily maximum temperatures fall to their lowest, about 84 °F (29 °C), in July. The average annual rainfall varies between 43 and 114 inches (1,100 and 2,900 mm), being highest on the windward northeast sides of the islands. Rain sinks so deeply into the hardened lava and porous rocks of Grande Comore that wells are difficult to drill. Traditionally, most of Grande Comore’s water supply has come from reservoirs filled in the rainy season and from freshwater springs along the coasts (foumbous). Source: https://www.britannica.com/place/Comoros  

2025/07/06

Republic of Malawi Day

Malawi, landlocked country in southeastern Africa. Endowed with spectacular highlands and extensive lakes, it occupies a narrow, curving strip of land along the East African Rift Valley. Lake Nyasa, known in Malawi as Lake Malawi, accounts for more than one-fifth of the country’s total area. Most of Malawi’s population engages in cash-crop and subsistence agriculture. The country’s exports consist of the produce of both small landholdings and large tea and tobacco estates. Malawi has received a significant amount of foreign capital in the form of development aid, which has contributed greatly toward the exploitation of its natural resources and has allowed Malawi to at times produce a food surplus. Nevertheless, its population has suffered from chronic malnutrition, high rates of infant mortality, and grinding poverty—a paradox often attributed to an agricultural system that has favoured large estate owners. Most Malawians reside in rural locations. The country’s few large urban centres include Lilongwe, the capital, and Blantyre, the seat of the country’s judiciary. Land Malawi stretches about 520 miles (840 km) from north to south and varies in width from 5 to 100 miles (10 to 160 km). It is bordered by Tanzania to the north, Lake Malawi to the east, Mozambique to the east and south, and Zambia to the west. Relief While Malawi’s landscape is highly varied, four basic regions can be identified: the East African (or Great) Rift Valley, the central plateaus, the highlands, and the isolated mountains. The East African Rift Valley—by far the dominant feature of the country—is a massive troughlike depression running through the country from north to south and containing Lake Malawi (north and central) and the Shire River valley (south). The lake’s littoral, situated along the western and southern shores and ranging from 5 to 15 miles (8 to 24 km) in width, covers almost one-tenth of the total land area and is dotted with swamps and lagoons. The Shire valley stretches some 250 miles (400 km) from the southern end of Lake Malawi at Mangochi to Nsanje at the Mozambique border and contains Lake Malombe at its northern end. The plateaus of central Malawi rise to elevations of 2,500 to 4,500 feet (760 to 1,370 metres) and lie just west of the Lake Malawi littoral; the plateaus cover about three-fourths of the total land area. The highland areas are mainly isolated tracts that rise as much as 8,000 feet (2,400 metres) above sea level. They comprise the Nyika, Viphya, and Dowa highlands and Dedza-Kirk mountain range in the north and west and the Shire Highlands in the south. The isolated massifs of Mulanje (which reach 9,849 feet [3,002 metres], the highest point in the country) and Zomba (which reach 6,846 feet [2,087 metres]) represent the fourth physical region. Surmounting the Shire Highlands, they descend rapidly in the east to the Lake Chilwa–Phalombe plain. Drainage and soils The major drainage system is that of Lake Malawi, which covers some 11,430 square miles (29,600 square km) and extends beyond the Malawi border. It is fed by the North and South Rukuru, Dwangwa, Lilongwe, and Bua rivers. The Shire River, the lake’s only outlet, flows through adjacent Lake Malombe and receives several tributaries before joining the Zambezi River in Mozambique. A second drainage system is that of Lake Chilwa, the rivers of which flow from the Lake Chilwa–Phalombe plain and the adjacent highlands. Soils, distributed in a complex pattern, are composed primarily of red earths, with brown soils and yellow gritty clays on the plateaus. Alluvial soils occur on the lakeshores and in the Shire valley, while other soil types include hydromorphic (excessively moist) soils, black clays, and sandy dunes on the lakeshore. Climate There are two main seasons—the dry season, which lasts from May to October, and the wet season, which lasts from November to April. Temperatures vary seasonally, and they tend to decrease on average with increasing elevation. Nsanje, in the Shire River valley, has a mean July temperature in the high 60s F (low 20s C) and an October mean in the mid-80s F (high 20s C), while Dedza, which lies at an elevation of more than 5,000 feet (1,500 metres), has a July mean in the high 50s F (mid-10s C) and an October mean in the high 60s F (low 20s C). On the Nyika Plateau and on the upper levels of the Mulanje massif, frosts are not uncommon in July. Annual precipitation levels are highest over parts of the northern highlands and on the Sapitwa peak of the Mulanje massif, where they are about 90 inches (2,300 mm); they are lowest in the lower Shire valley, where they range from 25 to 35 inches (650 to 900 mm). Plant and animal life The natural vegetation pattern reflects the country’s diversity in relief, soils, and climate. Savanna (grassy parkland) occurs in the dry lowland areas. Miombo woodlands—sparse, open deciduous woodland characteristic of dry parts of eastern Africa—are an important habitat, particularly for the country’s large mammal populations. Woodlands with species of acacia trees cover isolated, more fertile plateau sites and river margins. Grass-covered broad depressions, called madambo (singular: dambo), dot the plateaus. Grasslands and evergreen forests are found in conjunction on the highlands and on the Mulanje and Zomba massifs. However, Malawi’s natural vegetation has been altered significantly by human activities. Swamp vegetation has given way to agricultural species as swamps have been drained and cultivated. Much of the original woodland has been cleared, and, at the same time, forests of softwoods have been planted in the highland areas. High population density and intensive cultivation of the Shire Highlands have also hindered natural succession there, while wells have been sunk and rivers dammed to irrigate the dry grasslands for agriculture. Game animals abound only in the game reserves, where antelope, buffalo, elephants, leopards, lions, rhinoceroses, and zebras occur; hippopotamuses live in Lake Malawi. The lakes and rivers of Malawi contain hundreds of species and numerous families of fish. Lake Malawi is particularly renowned for its remarkable biodiversity—an enormous range of fish species inhabit the lake, most of them endemic—and its southern region, as part of Lake Malawi National Park, was designated a UNESCO World Heritage site in 1984. The most common and commercially significant fish found in Malawi include the endemic tilapia, or chambo (nest-building freshwater fish); catfish, or mlamba; and minnows, or matemba. The Ministry of Mines, Natural Resources, and Environmental Affairs is charged with the responsibility of ensuring the protection of Malawi’s environment, mainly through the implementation of the Environmental Management Act of 1996. Among the major concerns are efficient resource utilization, land degradation, deforestation, conservation of marine life, biodiversity, climate change, ozone layer protection, sewage, the pollution of water from agriculture runoff such as fertilizers, endangered species, and industrial pollution. The majority of pollution comes from greenhouse gas emissions, mostly from the usage of coal and charcoal, natural gas, and petroleum. People of Malawi - Ethnic groups and languages Ten major ethnic groups are historically associated with modern Malawi—the Chewa, Nyanja, Lomwe, Yao, Tumbuka, Sena, Tonga, Ngoni, Ngonde, and the Lambya/Nyiha. All the African languages spoken are Bantu languages. From 1968 to 1994, Chewa was the only national language; it is now one of the numerous languages used in print and broadcast media and is spoken by a majority of the population. In 1996 government policy indicated that education in grades 1–4 would be provided in the students’ mother tongue or vernacular language; from grade 5, the medium of instruction would be English, which, though understood by less than one-fifth of the population at independence in 1964, continues to be used widely in business, administrative and judicial matters, higher education, and elsewhere. Other major languages include Lomwe, Yao, and Tumbuka. More … Score: https://www.britannica.com/place/Malawi

2025/07/06

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