Archiwum
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
Czytaj więcej2024/10/10
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
Czytaj więcej2024/10/09
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.
Czytaj więcej2024/10/08
About Lesotho
Beautiful, culturally rich, safe, affordable and easily accessible from Durban and Johannesburg, mountainous Lesotho is a vastly underrated travel ...
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Independence Day of the Kingdom of Lesotho
Lesotho, country in Southern Africa. A scenic land of tall mountains and narrow valleys, Lesotho owes a long history of political autonomy to the mountains that surround it and protect it from encroachment. Since the Neolithic Period, the mountain kingdom was the domain of Khoisan-speaking hunter-gatherers. In the 19th century the Sotho, led by Moshoeshoe I, took control of the region. It remained independent until it became a British protectorate, one of three British High Commission Territories (the others being Bechuanaland [now Botswana] and Swaziland). Completely encircled by the Republic of South Africa but separated from it by forbidding mountain ranges, Lesotho has endured decades of turbulent politics, periodic economic crises, and grinding poverty since gaining its independence from Great Britain in 1966. Though culturally conservative in the main, the people of the country welcomed the modernization programs begun in the 1990s, which have brought new wealth to the country but at the cost of much environmental damage. Tourism and revenues from the country’s diamond industry have also helped to improve material conditions, and the capital, Maseru, has grown to become one of Southern Africa’s most attractive cities. Of these changes, Sotho writer Mpho ’M’Atsepo Nthunya remarks, Maybe if there is one day enough for the hunger to stop, we can stop being so jealous of one another. If the jealousy is no more, we can begin to have dreams for each other. Land The country forms an enclave within South Africa, bordering on three of the latter’s provinces—KwaZulu-Natal, Free State, and Eastern Cape. Like only two other independent states in the world (Vatican City and the Republic of San Marino), Lesotho is completely encircled by another country, on which it must depend for access to the outside world. Relief, drainage, and soils Two-thirds of Lesotho consists of mountains. The highest peak, Mount Ntlenyana, is 11,424 feet (3,482 metres) above sea level. The Drakensberg range forms the eastern boundary with KwaZulu-Natal. The Maloti spurs of the Drakensberg, running north and south, join the main range in the north, forming a plateau from 9,000 to 10,500 feet (2,700 to 3,200 metres) in elevation. This plateau, the centre of the cattle-raising and agricultural industries, is the source of South Africa’s two largest rivers—the eastward-flowing Tugela and the westward-flowing Orange—as well as tributaries of the Caledon (Mohokare). Three other important rivers in Lesotho are the Senqunyane in the centre of the country, the Kometspruit in the southwest, and the Matsoku in the northeast. The foothills, with elevations averaging between 6,000 and 7,000 feet (1,800 and 2,100 metres), descend in undulating slopes to the west, where the lowlands bordering Free State rise to elevations of 5,000 to 6,000 feet (1,500 to 1,800 metres). The mountain soils are of basaltic origin and are shallow but rich. The soils of the lowlands derive mainly from the underlying sandstone. Extensive erosion has severely damaged soils throughout the country. Climate Precipitation, brought by the prevailing winds, occurs mostly between October and April and is variable; the annual average is about 28 inches (710 mm), with amounts decreasing from east to west. Hail is a frequent summer hazard. Temperatures in the lowlands reach as high as 90 °F (32 °C) in the summer and plunge to 20 °F (−7 °C) in the winter. In the highlands the temperature range is much wider, and readings below 0 °F (−18 °C) are not unusual. Frost occurs widely in the winter, when the Maloti Mountains are usually snowcapped. Plant and animal life Lesotho is largely covered in grasses, although trees also appear on the landscape. Indigenous trees include Cape willows, cheche bush (used for fuel), and wild olives. Other willows and white poplars have been introduced into the country. There are numerous indigenous species of aloes, which are commonly found in the cooler, wet areas. Overgrazing, overutilization, and soil erosion have drastically depleted and altered the grasslands, reedbeds, and woody bush on the slopes. Reforestation schemes have been attempted but have met with limited success. In the mid-19th century, zebras, wildebeests, ostriches, and lions could be found in the country. However, hunting and deforestation have mostly eliminated the populations of large mammals; the last lion was killed in the 1870s. Smaller antelope and hares can still be found, and the hyrax, or dassie, is common. Sehlabathebe National Park in the southeastern highlands near Qacha’s Nek protects such birds as raptors and such mammals as mountain reedbuck and leopards. Lesotho is the last stronghold in Southern Africa of the magnificent bearded vulture, or lammergeier. Some rivers contain yellowfish and the rare Maloti minnow; trout and the North African catfish have also been introduced. People - Ethnic groups The Sotho (also known as Basotho) form the overwhelming majority of the country’s population. They were originally united by a common loyalty to the royal house of Moshoeshoe I, who founded the Sotho nation in the 19th century. Internally, divisions between different chiefdoms—and within the royal lineage itself—have had political significance, but externally a sense of Sotho nationhood and cultural unity remains strong. Lesotho is also home to a Zulu minority, a small population of Asian or mixed ancestry, and a European community that is dominated by expatriate teachers, missionaries, aid workers, technicians, and development advisers. Languages Except for English, all the main languages spoken in Lesotho are members of the Niger-Congo language family. Sotho (Sesotho), a Bantu language, is spoken by the majority of the population, though both Sotho and English are official languages in the country. Zulu is spoken by a small but significant minority. Phuthi, a dialect of Swati, and Xhosa are also spoken in parts of Lesotho. Religion of Lesotho Some four-fifths of the population profess Christianity, of which the largest denomination is Roman Catholic; other denominations include Lesotho Evangelical, Presbyterian, and Anglican. Independent churches are also present, together with Zionist sects (small African sects that blend Pentecostal Christianity and indigenous ritual belief). Other religions—including Islam, Hinduism, and Buddhism—are practiced by small percentages of the population, as are traditional religions. Some adherents of Christianity also embrace traditional religious beliefs. Settlement patterns The population density of Lesotho is high for an African state, despite the thinly settled areas of mountainous terrain. A large proportion of the population lives in the western lowlands, which have a much higher population density than the rest of the country as a whole: almost three-fourths of the population lives in the narrow corridor, only 25 miles (40 km) in width, that stretches along the Caledon River. Although not permanently inhabited, the mountain grasslands on the slopes of the high plateau and in the valleys provide summer grazing for sheep and cattle, tended by herders in isolated cattle posts. Some of the deep valleys, such as the Senqunyane, produce crops of wheat, peas, and beans. Since independence in 1966, there has been considerable population movement toward the capital city, Maseru. While Maseru is the largest city by far, smaller urban populations inhabit Maputsoe, Teyateyaneng, Mafeteng, and Hlotse. However, about three-fourths of the population is rural. Families and clans still cluster together as units in the numerous small rural villages, where social cohesion is strengthened by the persistence of clan and family loyalties. The villages range in size from one large family to four or five extended families, with an average of 30 to 50 nuclear families. The villages, situated on the plains and surrounded by aloes and trees, offer fine views of the rocky highlands. More … Score: https://www.britannica.com/place/Lesotho
Czytaj więcej2024/10/04