Independence Day of the Republic of Fiji

Fiji, country and archipelago in the South Pacific Ocean. It surrounds the Koro Sea about 1,300 miles (2,100 km) north of Auckland, New Zealand. The archipelago consists of some 300 islands and 540 islets scattered over about 1,000,000 square miles (3,000,000 square km). Of the 300 islands, about 100 are inhabited. The capital, Suva, is on the southeast coast of the largest island, Viti Levu (“Great Fiji”). Land of Fiji - Relief Fiji has a complex geologic history. Based on a submerged platform of ancient formation, the Fiji islands are largely the product of volcanic action, sedimentary deposit, and formations of coral. Viti Levu has an area of about 4,000 square miles (10,000 square km) and accounts for more than half of Fiji’s land area. A jagged dividing range running from north to south has several peaks above 3,000 feet (900 metres), including Tomanivi (formerly Mount Victoria), at 4,344 feet (1,324 metres) the highest point in Fiji. The main river systems—the Rewa, Navua, Sigatoka (Singatoka), and Ba (Mba)—all have their headwaters in the central mountain area. To the southeast and southwest, as well as to the south where the range divides, the mountains give way to plateaus and then lowlands. The coastal plains in the west, northwest, and southeast account for less than one-fifth of Viti Levu’s area but are the main centres of agriculture and settlement. Vanua Levu, the second largest island, has an area of about 2,140 square miles (5,540 square km). It is divided along its length by a mountain range with peaks rising to more than 3,000 feet. On the island’s northern coast, away from the mouth of the Dreketi (Ndreketi) River, the coastal plains are narrow. Most of the other islands, including the Lomaiviti, Lau, and Yasawa groups, are volcanic in origin, but, like the major islands, they are bounded by coral reefs, offshore rocks, and shoals that make the Koro Sea hazardous for navigation. Climate At Suva the average summer high temperature is in the mid-80s F (about 29 °C), and the average winter low is in the high 60s F (about 20 °C); temperatures typically are lower in elevated inland areas. All districts receive the greatest amount of rainfall in the season from November through March, during which time tropical cyclones (hurricanes) are also experienced perhaps once every two years. While rainfall is reduced in the east of the larger islands from April to October, giving an annual average of about 120 inches (3,000 mm) per year, it virtually ceases in the west, to give an annual rainfall that approaches 70 inches (about 1,800 mm), thus making for a sharp contrast in both climatic conditions and agriculture between east and west. Plant and animal life Almost half of Fiji’s total area remains forested, while dry grasslands are found in western areas of the large islands. Coconut palms are common in coastal areas, and almost all tropical fruits and vegetables can be grown. Much of the shoreline is composed of reefs and rocks, while mangrove swamps are found on eastern coasts. There are few white-sand swimming beaches and, because of the encircling reef, little surf. Most animals, including pigs, dogs, cattle, and a few horses, are domesticated. Mongooses, introduced to prey on snakes and rats, are often seen. People of Fiji - Ethnic groups Although the indigenous Fijian people are usually classified as ethnically Melanesian, their social and political organization is closer to that of Polynesia, and there has been a high level of intermarriage between Fijians from the Lau group of islands of eastern Fiji and the neighbouring Polynesian islands of Tonga. Indigenous Fijians make up more than half the population; about another two-fifths are people of Indian descent, most of whom are descendants of indentured labourers brought to work in the sugar industry. A small number of Indians, particularly in commerce and in professions such as medicine and law, are descended from free migrants. There are minorities of part-Europeans, Chinese, and Pacific Islanders who have origins outside Fiji. In the last group is the Polynesian population of the Fijian dependency of Rotuma—an island of 18 square miles (47 square km) located about 400 miles (645 km) north-northwest of Suva—and the Banabans. The latter were forced to leave their home island, Banaba, now part of Kiribati, after destruction during World War II made it uninhabitable. Many Banabans settled on Rabi (Rambi) Island, off the eastern coast of Vanua Levu. Languages and religion English, Fijian, and Fijian Hindi were given equal status as official languages by the 1997 constitution. The widely used Fijian language has many dialects; the one most commonly used is known as Bauan Fijian and comes from Bau (Mbau), an island that enjoyed political supremacy at the advent of colonial rule. Most people speak at least two languages, including English and the language of their own ethnic community. Almost all indigenous Fijians are Christian, mostly Methodist. Most Indians are Hindu, though a significant minority are Muslim. About one-tenth of the population is Roman Catholic, and there is a small Assemblies of God community. Settlement patterns There is little intermarriage between ethnic communities. While Suva has a very mixed population, the sugar-producing regions of Viti Levu and Vanua Levu have predominantly Indian populations. On the smaller islands and in less-developed rural areas of the larger islands, indigenous Fijians live in traditional villages. About half the population lives in urban areas. The three largest urban centres are on Viti Levu: Suva, in the southeast, with about one-fourth of Fiji’s total population; Nasinu, a suburb of Suva that experienced rapid growth in the late 20th and early 21st centuries; and Lautoka, in northwestern Viti Levu, the centre of the sugar industry and the location of a major port. Labasa (Lambasa), on Vanua Levu, is a centre for administration, services, and sugar production. Demographic trends The population of Fiji is young. More than one-fourth of the population is under the age of 15, and another one-fourth is between the ages of 15 and 29. For four decades after World War II, indigenous Fijians were outnumbered by Indians. However, after the government was overthrown in 1987, many Indians fled to Australia, New Zealand, and Canada, and Fijians regained a plurality. With rapid urbanization, especially on the fringes of Suva, came the emergence of squatter settlements and some social problems. The disparities of income between urban and rural workers, contrasting lifestyles within the urban areas, and high urban unemployment can be seen as factors that have contributed to both an escalating rate of crime and the rapid growth of a trade union movement. More … Score: https://www.britannica.com/place/Fiji-republic-Pacific-Ocean      

2025/10/10

Fiji Destination - Tourism Fiji

2025/10/09

Independence day of the Republic of Uganda

Independence day of the Republic of Uganda_opis Uganda, country in east-central Africa. About the size of Great Britain, Uganda is populated by dozens of ethnic groups. The English language and Christianity help unite these diverse peoples, who come together in the cosmopolitan capital of Kampala, a verdant city whose plan includes dozens of small parks and public gardens and a scenic promenade along the shore of Lake Victoria, Africa’s largest freshwater lake. The Swahili language unites the country with its East African neighbours Kenya and Tanzania. “Uganda is a fairy-tale. You climb up a railway instead of a beanstalk, and at the end there is a wonderful new world,” wrote Sir Winston Churchill, who visited the country during its years under British rule and who called it “the pearl of Africa.” Indeed, Uganda embraces many ecosystems, from the tall volcanic mountains of the eastern and western frontiers to the densely forested swamps of the Albert Nile River and the rainforests of the country’s central plateau. The land is richly fertile, and Ugandan coffee has become both a mainstay of the agricultural economy and a favourite of connoisseurs around the world.Uganda obtained formal independence on October 9, 1962. Its borders, drawn in an artificial and arbitrary manner in the late 19th century, encompassed two essentially different types of societies: the relatively centralized Bantu kingdoms of the south and the more decentralized Nilotic and Sudanic peoples to the north. The country’s sad record of political conflict, coupled with environmental problems and the ravages of a countrywide AIDS epidemic, hindered progress and growth for many years. Yet, even so, at the beginning of the 21st century a popularly elected civilian government ruled Uganda, which had attained political stability, had set an example for tackling the AIDS crisis that threatened to overwhelm the continent, and enjoyed one of the fastest-growing economies in Africa. Land of Uganda Uganda is bordered by South Sudan to the north, Kenya to the east, Tanzania and Rwanda to the south, and the Democratic Republic of the Congo to the west. The capital city, Kampala, is built around seven hills not far from the shores of Lake Victoria, which forms part of the frontier with Kenya and Tanzania. Relief Most of Uganda is situated on a plateau, a large expanse that drops gently from about 5,000 feet (1,500 metres) in the south to approximately 3,000 feet (900 metres) in the north. The limits of Uganda’s plateau region are marked by mountains and valleys. To the west a natural boundary is composed of the Virunga (Mufumbiro) Mountains, the Ruwenzori Range, and the Western Rift Valley (see East African Rift System). The volcanic Virunga Mountains rise to 13,540 feet (4,125 metres) at Mount Muhavura and include Mount Sabinio (11,959 feet [3,645 metres]), where the borders of Uganda, the Democratic Republic of the Congo, and Rwanda meet. Farther north the Ruwenzori Range—popularly believed to be Ptolemy’s Mountains of the Moon—rises to 16,762 feet (5,109 metres) at Margherita Peak, Uganda’s highest point; its heights are often hidden by clouds, and its peaks are capped by snow and glaciers. Between the Virunga and Ruwenzori mountains lie Lakes Edward and George. The rest of the boundary is composed of the Western Rift Valley, which contains Lake Albert and the Albert Nile River.The northeastern border of the plateau is defined by a string of volcanic mountains that include Mounts Morungole, Moroto, and Kadam, all of which exceed 9,000 feet (2,750 metres) in elevation. The southernmost mountain—Mount Elgon—is also the highest of the chain, reaching 14,178 feet (4,321 metres). South and west of these mountains is an eastern extension of the Rift Valley, as well as Lake Victoria. To the north the plateau is marked on the South Sudanese border by the Imatong Mountains, with an elevation of about 6,000 feet (1,800 metres). Drainage Uganda’s Lake Victoria (26,828 square miles [69,484 square km]), in the southeastern part of the country, is the world’s second largest inland freshwater lake by size after Lake Superior in North America, although Lake Baikal in Siberia is larger by volume and depth. Victoria is also one of the sources of the Nile River. Five other major lakes exist in the country: Edward and George to the southwest; Albert to the west; Kyoga in central Uganda; and Bisina in the east. Together with the lakes, there are eight major rivers. These are the Victoria Nile in central Uganda; the Achwa, Okok, and Pager in the north; the Albert Nile in the northwest; and the Kafu, Katonga, and Mpongo in the west.The southern rivers empty into Lake Victoria, the waters of which escape through Owen Falls near Jinja and form the Victoria Nile. This river flows northward through the eastern extension of Lake Kyoga. It then turns west and north to drop over Karuma Falls and Murchison Falls before emptying into Lake Albert.Lake Albert is drained to the north by the Albert Nile, which is known as the Al-Jabal River, or Mountain Nile, after it enters South Sudan at Nimule. Rivers that rise to the north of Lake Victoria flow into Lake Kyoga, while those in the southwest flow into Lakes George and Edward. Except for the Victoria and Albert Niles, the rivers are sluggish and often swampy. Clear streams are found only in the mountains and on the slopes of the Rift Valley. Most of the rivers are seasonal and flow only during the wet season, and even the few permanent rivers are subject to seasonal changes in their rates of flow. Soils The soils, in general, are fertile (and primarily lateritic), and those in the region of Lake Victoria are among the most productive in the world. Interspersed with these are the waterlogged clays characteristic of the northwest and of the western shores of Lake Victoria. Climate The tropical climate of Uganda is modified by elevation and, locally, by the presence of the lakes. The major air currents are northeasterly and southwesterly. Because of Uganda’s equatorial location, there is little variation in the sun’s declination at midday, and the length of daylight is nearly always 12 hours. All of these factors, combined with a fairly constant cloud cover, ensure an equable climate throughout the year. Most parts of Uganda receive adequate precipitation; annual amounts range from less than 20 inches (500 mm) in the northeast to a high of 80 inches (2,000 mm) in the Sese Islands of Lake Victoria. In the south, two wet seasons (April to May and October to November) are separated by dry periods, although the occasional tropical thunderstorm still occurs. In the north, a wet season occurs between April and October, followed by a dry season that lasts from November to March. More … Score: https://www.britannica.com/place/Uganda  

2025/10/09

Fly over Africa: The Republic of Uganda

Uganda has transformed itself from a country with a troubled past to one of relative stability and prosperity. With its dense forests, glassy lakes and sprawling savannas, Uganda is a highlight reel of the African landscape.

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Beauty Of Turkmenistan

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Independence day Republic of Guinea-Bissau

Guinea-Bissau, country of western Africa. Situated on the Atlantic coast, the predominantly low-lying country is slightly hilly farther inland. The name Guinea remains a source of debate; it is perhaps a corruption of an Amazigh (Berber) word meaning “land of the blacks.” The country also uses the name of its capital, Bissau, to distinguish it from Guinea, its neighbour to the east and south. In the 15th and early 16th centuries the Portuguese commanded the entire western coast of Africa. Gradually their monopoly gave way to incursions by French, Dutch, English, and other European powers. The French pressured both the northern and southern borders of what is now Guinea-Bissau and placed the Casamance region of southern Senegal fully under French rule after the late 19th century. The English rivaled Portuguese authority on the coast, particularly at Bolama; a long-running dispute between the two powers resulted with Guinea-Bissau under Portuguese rule. Although Bissau is the country’s present capital and largest city, the towns of Bolama and Cacheu were important during the slave trade and in the colonial era. Land Guinea-Bissau is bounded by Senegal to the north, Guinea to the east and south, and the Atlantic Ocean to the west. It includes the Bijagós (Bissagos) archipelago and other islands that lie off the coast. Relief Almost all of Guinea-Bissau is low-lying and bathed daily by tidal waters that reach as far as 62 miles (100 km) inland. In the southeastern part of the country, the Fouta Djallon plateau rises approximately 600 feet (180 metres). The Boé Hills extend from the western slopes of the Fouta Djallon to the Corubal basin and the Gabú Plain. Drainage and soils The coastal area is demarcated by a dense network of drowned valleys called rias. The Bafatá Plateau is drained by the Geba and Corubal rivers. The Gabú Plain occupies the northeastern portion of the country and is drained by the Cacheu and Geba rivers and their tributaries. The interior plains are part of the southern edge of the Sénégal River basin. The uniform elevation of the mature floodplain allows rivers to meander and renders the area susceptible to flooding during the rainy season. Some eastern portions of Guinea-Bissau form a part of the upper basin of the Gambia River system. Tidal penetration into the interior, facilitated by Guinea-Bissau’s flat coastal topography, carries some agricultural advantage: the surge of brackish water can be used to irrigate the extensive drowned rice paddies called bolanhas. Anti-colonial warfare had a devastating effect on Guinea-Bissau’s soils. Arable land that fell out of use was subject to soil erosion, and, with the destruction of protective riverine dikes, the arability of some soils was compromised by excessive salination. Climate Guinea-Bissau has a generally tropical climate influenced by the intertropical convergence zone (ITCZ), a belt of converging trade winds that circles the Earth near the Equator. There are two pronounced seasons: the hot, rainy season, which usually lasts from June to November, and the hot, dry season. April and May are the hottest months, and temperatures can reach the high 90s F (mid-30s C). Precipitation does not vary greatly by elevation in Guinea-Bissau, although it does vary between coastal and inland areas; the coast receives some 60 to 120 inches (1,500 to 3,000 mm) of precipitation, whereas the interior is influenced by the tropical savanna climate, with greater variation in precipitation and temperature. Plant and animal life Guinea-Bissau’s three ecological zones—the tidal estuaries, the heavily forested interior plain, and the savanna—are home to remarkably diverse flora and fauna. Aquatic and riverine birds such as flamingos and pelicans are especially numerous in the coastal swamps, which are also inhabited by a variety of reptiles such as snakes, crocodiles, and sea turtles, the latter of which are endangered. In the plains and forests, lizards, gazelles, antelopes, monkeys and apes, parrots, hyenas, and leopards abound. Although there was once a substantial elephant population, it has since been virtually eliminated. Many wild animals are hunted for their meat and hides. People - Ethnic and linguistic groups Guinea-Bissau’s population is dominated by more than 20 African ethnicities, including the Balante, one of the largest ethnic groups in the country, the numerous Fulani and their many subgroups, the Diola, the Nalu, the Bijagó, the Landuma, the Papel (Pepel), and the Malinke. There is also a small Cape Verdean minority with mixed African, European, Lebanese, and Jewish origins. During the colonial period the European population consisted mainly of Portuguese but also included some Lebanese, Italian, French, and English groups, as well as members of other nationalities. Notably, there was never a substantial settler population in Guinea-Bissau, as there was in other Portuguese colonies. Among the African languages spoken in Guinea-Bissau, some 20 languages and dialects classified in the Atlantic and Mande branches of Niger-Congo languages predominate. Although Portuguese is the country’s official and formal language, it is Crioulo—a creole that emerged during the slave trade—that is spoken as the lingua franca and exerts a unifying influence in the rural areas. Religion About two-fifths of the population is Muslim. Among Christians, who make up about one-fifth of the population, Roman Catholicism predominates. About one-sixth of the population practices traditional beliefs, which include ancestor worship, possession, and animism and are especially prevalent along the coast and in the central regions. Christianity and Islam are enriched with African traditional beliefs, which results in a unique religious syncretism; saints’ days, for example, may be celebrated with drumming, processionals, masks, and traditional dance. Settlement patterns Most of the population of Guinea-Bissau live in small villages and the country’s several main towns. The population is sparse on the low-lying lands of the coast and in the savanna regions. The majority of Guinea-Bissau’s population traditionally lived in rural villages and individual households. From 1963 to 1974, during the armed struggle for independence, about one-third of the rural population fled to neighbouring countries for refuge. Those who remained tried to restructure their lives in liberated zones, while the colonial military imposed a system of aldeamentos, concentrated settlements designed to isolate the population from the nationalist forces. Although migration to urban centres such as Bissau, Cacheu, and Bolama had generally been increasing since independence, much of the urban population fled during the fighting that erupted in the late 1990s. About half of the population is rural. Demographic trends Population growth in Guinea-Bissau is lower than that of the rest of the African continent. Life expectancy for both men and women is well below the African average and substantially lower than the world average, and infant mortality is high. The population of Guinea-Bissau is, on the whole, very young: about two-fifths of the population is under age 15 and about two-thirds under 30. Guinea-Bissau does not have a significant expatriate population living outside the country, except those in the neighbouring countries of Guinea and Senegal. Historically, the only traditional pattern of emigration was due to human trafficking; during the 15th through 19th century, thousands of Guineans were exported to Cape Verde and the New World, especially to Cuba and the northern Brazilian states of Grão Pará and Maranhão, as slaves or indentured servants. More: Score: https://www.britannica.com/place/Guinea-Bissau

2025/09/24

Belize Tourism Board: BTB

Learn about Belize's Cruise Ports, Passenger tips or download our Cruise brochure. read more. TOUR OPERATORS. Apply or renew your Tour Operator License ...

2025/09/23