Wernisaż wystawy "Ludobójstwo Ormian: Relacje na pierwszych stronach prasy światowej"

Zapraszamy Was serdecznie na wernisaż wystawy "Ludobójstwo Ormian: Relacje na pierwszych stronach prasy światowej" w Centrum Wielokulturowym, w ramach którego wirtualnie spotykamy się z Samvelem Mkrtchianem, Ambasadorem Republiki Armenii w Polsce.

2021/04/27

Togolese Republic Independence Day

Togo, country of western Africa. Lomé, the capital, is situated in the southwest of the country and is the largest city and port. Until 1884 what is now Togo was an intermediate zone between the states of Asante and Dahomey, and its various ethnic groups lived in general isolation from each other. In 1884 it became part of the Togoland German protectorate, which was occupied by British and French forces in 1914. In 1922 the League of Nations assigned eastern Togoland to France and the western portion to Britain. In 1946 the British and French governments placed the territories under United Nations trusteeship (see Trusteeship Council). Ten years later British Togoland was incorporated into the Gold Coast, and French Togoland became an autonomous republic within the French Union. Togo gained independence in 1960. The economy rests largely on agriculture, although the country’s extensive phosphate reserves are also significant. Land From its 32-mile (51-km) coastline on the Gulf of Guinea, Togo extends northward for about 320 miles (515 km) between Ghana to the west and Benin to the east to its boundary with Burkina Faso in the north. Relief, drainage, and soils Togo consists of six geographic regions. The low-lying, sandy beaches of the narrow coastal region are backed by tidal flats and shallow lagoons, the largest of which is Lake Togo. Beyond the coast lies the Ouatchi Plateau, which stretches about 20 miles (32 km) inland at an elevation of some 200 to 300 feet (60 to 90 metres). This is the region of the so-called terre de barre, a lateritic (reddish, leached, iron-bearing) soil. Northeast of the plateau is a tableland, the highest elevations reaching 1,300 to 1,500 feet (400 to 460 metres). This region is drained by the Mono River and its tributaries, including the Ogou, and other smaller rivers. West and southwest of the tableland the terrain gradually rises toward the Togo Mountains, also known as the Togo-Atakora Mountains, which run across central Togo from the south-southwest to the north-northeast. Part of a chain that begins in the Akwapim Hills of Ghana (see Akwapim-Togo ranges), the range ends in Benin, where it is known as the Atakora Mountains. Mount Agou (Baumann Peak), which rises to about 3,235 feet (986 metres), is the highest mountain in Togo. Beyond the Togo Mountains to the north lies the Oti River sandstone plateau. This is a savanna region drained by the Oti River, one of the main tributaries of the Volta. To the far northwest is a higher region of granite and gneiss; the cliffs of Dapaong (Dapango) are located in this region. Climate Togo has a tropical climate. In the south the rainy seasons occur from mid-April through June and from mid-September through October. The narrow coastal zone, which receives about 35 inches (890 mm) of precipitation annually, is the driest region. The area near Palimé, about 65 miles (100 km) inland, receives the highest amount of precipitation—about 70 inches (1,800 mm) annually. The north has only one rainy season, when precipitation averages about 45 inches (1,150 mm), mostly falling from June to the end of September; during the rest of the year the warm, dry harmattan (a dust-laden wind) predominates. Mean annual temperatures vary from the high 70s F (mid-20s C) along the coast and in the mountains to the low 80s F (high 20s C) on the northern plateau. Daily minimum temperatures reaching the high 60s F (low 20s C) are recorded in the mountains in August. Daily maxima in the low 100s F (high 30s C) occur in the north during March and April at the end of the long dry season. Plant and animal life Savanna-type vegetation is predominant in Togo. On the southern plateaus large trees, including the baobab, are common, but they are rare in the north. The southwestern highland regions are covered with tropical forests, also found along the river valleys. The coastal zone is dotted with mangrove and reed swamps. Wild animals are not found in great numbers, especially in the southern and central regions. A few lions, leopards, and elephants can be seen in the north. Monkeys, snakes, and lizards are numerous in many areas, and crocodiles and hippopotamuses abound in the rivers. In the Keran Forest Reserve near Sansanné-Mango in the north, there are wild herds of buffalo, asses, warthogs, antelope, and deer. Numerous species of birds and insects are found in the country. Fish caught off the coast include mackerel, bass, seabream, red snapper, triggerfish, dorado, ray, and sole, while crustaceans include shrimp and lobster. People Ethnic groups and languages The population of Togo is made up of about 30 ethnic groups, many of whom are immigrants from other parts of western Africa. The groups indigenous to Togo live in the north and southwest. The northern groups include the following Gur-speaking peoples: the Gurma; the Natimba, Dye, and Konkomba; the Tamberma; the Basari; the Moba; the Losso (Naudem); the Kabre and Logba; and the Lamba (Namba); a small number of Atlantic-speaking Fulani; and the Kebu (Akebu). In the southwest the indigenous Kwa peoples also belonging to the central Togo group are the Kposo (Akposso), the Adele, and the Ahlo. The Ewe, who emigrated from Nigeria between the 14th and 16th century, form the major ethnic group. There are also some scattered Yoruba, mainly Ana. Groups who emigrated from present-day Ghana and Côte d’Ivoire since the 17th century include the Mina (Ga and Ané), the Ga-Dangme, the Kpelle and the Anyama, the Chakosi, and the Dagomba. The northern groups—the Kotokoli (or Temba), Gurma, and Mossi—entered mainly from Burkina Faso.Most of the country’s non-Africans—the majority of whom are French—live in Lomé. Brazilians, or Portuguese of Brazilian birth, constituted the original trading settlement in Togo, and today African-Brazilians are closely associated with economic and political development. The official language is French, although it is not widely spoken outside of business and government. Widely spoken indigenous languages belong to the Niger-Congo language family and include Ewe in the south and Kabiye in the north. More …. Score: https://www.britannica.com/place/Togo

2021/04/27

King's Day Kingdom of the Netherlands

Netherlands, country located in northwestern Europe, also known as Holland. “Netherlands” means low-lying country; the name Holland (from Houtland, or “Wooded Land”) was originally given to one of the medieval cores of what later became the modern state and is still used for 2 of its 12 provinces (Noord-Holland and Zuid-Holland). A parliamentary democracy under a constitutional monarch, the kingdom includes its former colonies in the Lesser Antilles: Aruba, Bonaire, Curaçao, Saba, Sint Eustatius, and Sint Maarten. The capital is Amsterdam and the seat of government The Hague. The country is indeed low-lying and remarkably flat, with large expanses of lakes, rivers, and canals. Some 2,500 square miles (6,500 square km) of the Netherlands consist of reclaimed land, the result of a process of careful water management dating back to medieval times. Along the coasts, land was reclaimed from the sea, and, in the interior, lakes and marshes were drained, especially alongside the many rivers. All this new land was turned into polders, usually surrounded by dikes. Initially, man power and horsepower were used to drain the land, but they were later replaced by windmills, such as the mill network at Kinderdijk-Elshout, now a UNESCO World Heritage site. The largest water-control schemes were carried out in the second half of the 19th century and in the 20th century, when steam pumps and, later, electric or diesel pumps came into use.Despite government-encouraged emigration after World War II, which prompted some 500,000 persons to leave the country, the Netherlands is today one of the world’s most densely populated countries. Although the population as a whole is “graying” rapidly, with a high percentage over age 65, Amsterdam has remained one of the liveliest centres of international youth culture. There, perhaps more than anywhere else in the country, the Dutch tradition of social tolerance is readily encountered. Prostitution, “soft-drug” (marijuana and hashish) use, and euthanasia are all legal but carefully regulated in the Netherlands, which was also the first country to legalize same-sex marriage. This relative independence of outlook was evident as early as the 16th and 17th centuries, when the Dutch rejected monarchical controls and took a relatively enlightened view of other cultures, especially when they brought wealth and capital to the country’s trading centres. In that period Dutch merchant ships sailed the world and helped lay the foundations of a great trading country characterized by a vigorous spirit of enterprise. In later centuries, the Netherlands continued to have one of the most advanced economies in the world, despite the country’s modest size. The Dutch economy is open and generally internationalist in outlook. With Belgium and Luxembourg, the Netherlands is a member of the Benelux economic union, which in the 1950s and 1960s served as a model for the larger European Economic Community (EEC; now embedded in the European Union [EU]), of which the Benelux countries are members. The Netherlands is also a member of the North Atlantic Treaty Organization (NATO) and the Organisation for Economic Co-operation and Development (OECD), and it plays host to a number of international organizations, especially in the legal sector, such as the International Court of Justice. Get a Britannica Premium subscription and gain access to exclusive content. Subscribe Now The Dutch reputation for tolerance was tested in the late 20th and early 21st centuries, when an increase in immigration from non-European Union countries and a populist turn in politics resulted in growing nationalism and even xenophobia, marked by two race-related political assassinations, in 2002 and 2004, and the government’s requirement that immigrants pass an expensive ‘‘integration’’ test before they enter the country. Land Relief The Netherlands is bounded by the North Sea to the north and west, Germany to the east, and Belgium to the south. If the Netherlands were to lose the protection of its dunes and dikes, the most densely populated part of the country would be inundated (largely by the sea but also in part by the rivers). This highly developed part of the Netherlands, which generally does not lie higher than about three feet (one metre) above sea level, covers more than half the total area of the country. About half of this area (more than one-fourth of the total area of the country) actually lies below sea level. The lower area consists mainly of polders, where the landscape not only lies at a very low elevation but is also very flat in appearance. On such land, building is possible only on “rafts,” or after concrete piles, sometimes as long as 65 feet (20 metres), have been driven into the silt layer. In the other, higher area, the layers of sand and gravel in the eastern part of the country were pushed sideways and upward in some places by ice tongues of the Saale Glacial Stage, forming elongated ridges that may reach a height of more than 330 feet (100 metres) and are the principal feature of the Hoge Park Veluwe National Park. The only part of the country where elevations exceed 350 feet (105 metres) is the border zone of the Ardennes. The Netherlands’ highest point, the Vaalserberg, in the extreme southeastern corner, rises to 1,053 feet (321 metres). Drainage and dikes The Zuiderzee was originally an estuary of the Rhine River. By natural action it then became a shallow inland sea, biting deep into the land, and eventually it was hollowed into an almost circular shape by the action of winds and tides. In 1920 work was begun on the Zuiderzee project, of which the IJsselmeer Dam (Afsluitdijk), begun in 1927, was a part. This 19-mile- (30-km-) long dam was completed in 1932 to finally seal off the Zuiderzee from the Waddenzee and the North Sea. In the IJsselmeer, or IJssel Lake, formed from the southern part of the Zuiderzee, four large polders, the IJsselmeer Polders, with a total area of about 650 square miles (1,700 square km), were constructed around a freshwater basin fed by the IJssel and other rivers and linked with the sea by sluices and locks in the barrier dam. The first two polders created there—Wieringermeer and North East (Noordoost) Polder, drained before and during World War II—are used mostly for agriculture. The two polders reclaimed in the 1950s and ’60s—South Flevoland Polder (Zuidelijk) and East Flevoland Polder (Oostelijk)—are used for residential, industrial, and recreational purposes. Among the cities that have developed there are Lelystad and Almere.In the southwest, the disastrous gales and spring tide of February 1, 1953, which flooded some 400,000 acres (162,000 hectares) of land and killed 1,800 people, accelerated the implementation of the Delta Project, which aimed to close off most of the sea inlets of the southwestern delta. These delta works were designed to shorten the coastline by 450 miles (725 km), combat the salination of the soil, and allow the development of the area through roads that were constructed over 10 dams and 2 bridges built between 1960 and 1987. The largest of these dams, crossing the five-mile- (eight-km-) wide Eastern Schelde (Oosterschelde) estuary, has been built in the form of a storm-surge barrier incorporating dozens of openings that can be closed in the event of flood. The barrier is normally open, allowing salt water to enter the estuary and about three-fourths of the tidal movement to be maintained, limiting damage to the natural environment in the Eastern Schelde. In the interest of the commerce of the ports of Rotterdam and Antwerp, no dams were constructed in the New Waterway, which links Rotterdam to the North Sea, or the West Schelde, an approach to Antwerp, Belgium. The dikes along these waterways consequently had to be strengthened. A region with a very specific character has been formed by the great rivers—Rhine, Lek, Waal, and Maas (Meuse)—that flow from east to west through the central part of the country. The landscape in this area is characterized by high dikes along wide rivers, orchards along the levees formed by the rivers, and numerous large bridges over which pass the roads and railways that connect the central Netherlands with the southern provinces. More …. Score: https://www.britannica.com/place/Netherlands

2021/04/27

Republic of Sierra Leone Independence Day

Sierra Leone, country of western Africa. The country owes its name to the 15th-century Portuguese explorer Pedro de Sintra, the first European to sight and map Freetown harbour. The original Portuguese name, Serra Lyoa (“Lion Mountains”), referred to the range of hills that surrounds the harbour. The capital, Freetown, commands one of the world’s largest natural harbours. Although most of the population is engaged in subsistence agriculture, Sierra Leone is also a mining centre. Its land yields diamonds, gold, bauxite, and rutile (titanium dioxide). Internal conflict crippled the country from the late 1980s onward, culminating in a brutal civil war that took place from 1991 to 2002. Since the end of the war, the government of Sierra Leone has undergone the arduous task of rebuilding the country’s physical and social infrastructure while fostering reconciliation. Relief Sierra Leone is bordered on the north and east by Guinea, on the south by Liberia, and on the west by the Atlantic Ocean. The country can be divided into four distinct physical regions: the coastal swamp, the Sierra Leone Peninsula, the interior plains, and the interior plateau and mountain region. The coastal swamp region extends along the Atlantic for about 200 miles (320 km). It is a flat, low-lying, and frequently flooded plain that is between 5 and 25 miles (8 and 40 km) wide and is composed mainly of sands and clays. Its numerous creeks and estuaries contain mangrove swamps. Sandbars, generally separated by silting lagoons, sometimes form the actual coast. The Sierra Leone Peninsula, which is the site of Freetown, is a region of thickly wooded mountains that run parallel to the sea for about 25 miles (40 km). The Peninsula Mountains rise from the coastal swamps and reach some 2,900 feet (880 metres) at Picket Hill. Get a Britannica Premium subscription and gain access to exclusive content. Subscribe Now Inland from the coastal plain is the interior plains region. In the north it comprises featureless seasonal swamps known as “Bolilands” (boli being a Temne word for those lands that are flooded in the rainy season and dry and hard in the dry season and on which only grass can grow). In the south the plains comprise rolling wooded country where isolated hills rise abruptly to more than 1,000 feet (300 metres). The interior contains a variety of landforms ranging from savanna-covered low plains to rocky scarp and hill country. The interior plateau and mountain region, encompassing roughly the eastern half of the country, is composed mainly of granite with a thick laterite (iron-bearing) crust; to the west it is bounded by a narrow outcrop of mineral-bearing metamorphic rocks known as the Kambui Schists. Rising above the plateau are a number of mountain masses; in the northeast the Loma Mountains are crowned by Mount Loma Mansa (Mount Bintimani) at 6,391 feet (1,948 metres), and the Tingi Mountains rise to 6,080 feet (1,853 metres) at Sankanbiriwa Peak. Numerous narrow inland valley swamps associated with the river systems occur in this region. Drainage The country’s drainage pattern is dense. Numerous rivers rise in the well-watered Fouta Djallon highlands of Guinea and flow in a general northeast-to-southwest direction across Sierra Leone. Their middle courses are interrupted by rapids that restrict navigability to only a short distance inland. River levels show considerable seasonal fluctuations. The drainage system has nine major rivers and a series of minor coastal creeks and tidal streams. From north to south the principal rivers are the Great Scarcies (also called the Kolenté), Little Scarcies, Rokel (also called the Seli; known in its lower course where it meets the Atlantic as the Sierra Leone River), Gbangbaia, Jong, Sewa, Waanje, Moa, and Mano. The Great Scarcies, Moa, and Meli (one of the Moa’s tributaries) form portions of the border with Guinea, while the Mano forms much of the country’s frontier with Liberia. The river basins range in size from 5,460 square miles (14,140 square km) for the Sewa to less than 385 square miles (1,000 square km) for the smaller basins. Soils In most areas the dominant soils are of the weathered and leached lateritic type. Red to yellow-brown in colour, they contain oxides of iron and aluminum and are acid. Kaolin (china) clays are important in some areas; when cultivated, they are light, readily workable, and free-draining, with productivity that depends largely on the nutrients provided by the vegetation previously cleared and burned. In the coastal plains, lateritic soils that have developed on sandy deposits are agriculturally poor, but those derived from basic igneous rocks are somewhat better. Swamp soils occur over large areas on the coastal plains where drainage is a problem. In coastal and estuarine areas where mangrove is the natural vegetation, productive soils can be acquired by clearance, but careful water control is sometimes needed to prevent toxicity. At the foot of the main escarpment, on the Sula Mountain plateau, and elsewhere an iron-rich laterite crust forms a surface that is intractable for agricultural production. Climate The climate is tropical and is characterized by the alternation of rainy and dry seasons. Conditions are generally hot and humid. Mean monthly temperatures range from the upper 70s F (mid-20s C) to the low 80s F (upper 20s C) in low-lying coastal areas; inland they may range from the low to mid-70s F (low 20s C) to the low 80s F. In the northeast, where extremes of temperature are greater, mean daily minimums fall to the mid-50s F (low to mid-10s C) in January, and mean daily maximums rise to the low 90s F (low 30s C) in March. During the rainy season, from May to October, humid air masses from the Atlantic dominate. The sky is cloudy, the winds are southwesterly, sunshine is minimal, and rain falls almost daily, especially during July and August. Precipitation is greater on the coast than inland; the Peninsula Mountains receive more than 200 inches (5,000 mm) annually, while the northeast receives about 80 inches (2,000 mm) a year. The dry season, from November to April, is characterized by the harmattan, a hot, dry wind that blows from the Sahara. The rainy season tends to have cooler daily maximum temperatures than the dry season by about 10 °F (6 °C). The relative humidity, however, may be as high as 90 percent for considerable periods, particularly during the wettest months, from July to September. Plant and animal life The distribution of plants and animals has been influenced by such factors as relief and soil types and, perhaps more important, by farming methods and civil strife. Remnants of the extensive original forest cover survive in the Gola Forest Reserves, in the southeastern hill country near the Liberian border. Secondary forest is now dominant; valuable timber species including African mahogany and African teak, once common in the original forests, are now rare. The secondary forest consists of other tree species such as the fire-resistant palm tree, a valuable source of palm oil and kernels. The prevalence of savanna vegetation increases to the north as precipitation decreases. The savannas owe their present extent and character largely to the erosion produced by farming, grazing, and the use of fire. There are some small areas of climax savanna—a closed area of broad-leaved, low-growing trees and tall tussocky grasses. Other savannas are derived from forest and are characterized by fire-resistant savanna trees with tall grasses. Tracts of tallgrass savanna also occur. Remnants of mangrove swamps constitute the main coastal vegetation community, especially in the saline tidal areas of river estuaries. Piassava, a kind of raffia palm, is common in the swampy grasslands of the south. Unrestricted hunting during Sierra Leone’s civil war (1991–2002) adversely affected much of the country’s wildlife. Large game animals, such as elephants, leopards, lions, hyenas, and buffalo, are rarely seen outside of national parks or reserves. Chimpanzees and various species of monkeys are common in the forest zones, while other animals, such as antelope and bushpigs, are more generally distributed. There is a wide variety of insects, including the malaria-carrying mosquito and the tsetse fly. Hippopotamuses, crocodiles, and manatees occupy the rivers, including such rare species as the pygmy hippopotamus and the dwarf crocodile. The coastal waters, estuaries, and rivers, such as the Sierra Leone and the Sherbro, contain a wide variety of fish and shellfish, such as tuna, barracuda, bonga (shad), snapper, herring, mackerel, and lobster. Sierra Leone’s rich birdlife, which emerged relatively unscathed from the years of conflict, includes emerald cuckoos, owls, little African swift, vultures, and many other species. Several parks, sanctuaries, and reserves have been established to protect Sierra Leone’s wildlife, including Tiwai Island Wildlife Sanctuary and the Gola Forest Reserves in the south and Outamba-Kilimi National Park in the north. Tacugama Chimpanzee Sanctuary, located near Freetown, was established to rescue and rehabilitate abandoned or orphaned chimpanzees. More …. Score: https://www.britannica.com/place/Sierra-Leone

2021/04/27

Freedom Day OF South Africa

South Africa, the southernmost country on the African continent, renowned for its varied topography, great natural beauty, and cultural diversity, all of which have made the country a favoured destination for travelers since the legal ending of apartheid (Afrikaans: “apartness,” or racial separation) in 1994. South Africa’s remoteness—it lies thousands of miles distant from major African cities such as Lagos and Cairo and more than 6,000 miles (10,000 km) away from most of Europe, North America, and eastern Asia, where its major trading partners are located—helped reinforce the official system of apartheid for a large part of the 20th century. With that system, the government, controlled by the minority white population, enforced segregation between government-defined races in housing, education, and virtually all spheres of life, creating in effect three nations: one of whites (consisting of peoples primarily of British and Dutch [Boer] ancestry, who struggled for generations to gain political supremacy, a struggle that reached its violent apex with the South African War of 1899–1902); one of Blacks (consisting of such peoples as the San hunter-gatherers of the northwestern desert, the Zulu herders of the eastern plateaus, and the Khoekhoe farmers of the southern Cape regions); and one of “Coloureds” (mixed-race people) and ethnic Asians (Indians, Malays, Filipinos, and Chinese). The apartheid regime was disdained and even vehemently opposed by much of the world community, and by the mid-1980s South Africa found itself among the world’s pariah states, the subject of economic and cultural boycotts that affected almost every aspect of life. During this era the South African poet Mongane Wally Serote remarked,There is an intense need for self-expression among the oppressed in our country. When I say self-expression I don’t mean people saying something about themselves. I mean people making history consciously….We neglect the creativity that has made the people able to survive extreme exploitation and oppression. People have survived extreme racism. It means our people have been creative about their lives. Eventually forced to confront the untenable nature of ethnic separatism in a multicultural land, the South African government of F.W. de Klerk (1989–94) began to repeal apartheid laws. That process in turn set in motion a transition toward universal suffrage and a true electoral democracy, which culminated in the 1994 election of a government led by the Black majority under the leadership of the long-imprisoned dissident Nelson Mandela. As this transition attests, the country has made remarkable progress in establishing social equity in a short period of time. South Africa has three cities that serve as capitals: Pretoria (executive), Cape Town (legislative), and Bloemfontein (judicial). Johannesburg, the largest urban area in the country and a centre of commerce, lies at the heart of the populous Gauteng province. Durban, a port on the Indian Ocean, is a major industrial centre. East London and Port Elizabeth, both of which lie along the country’s southern coast, are important commercial, industrial, and cultural centres. Today South Africa enjoys a relatively stable mixed economy that draws on its fertile agricultural lands, abundant mineral resources, tourist attractions, and highly evolved intellectual capital. Greater political equality and economic stability, however, do not necessarily mean social tranquility. South African society at the start of the 21st century continued to face steep challenges: rising crime rates, ethnic tensions, great disparities in housing and educational opportunities, and the AIDS pandemic. Land South Africa is bordered by Namibia to the northwest, by Botswana and Zimbabwe to the north, and by Mozambique and Swaziland to the northeast and east. Lesotho, an independent country, is an enclave in the eastern part of the republic, entirely surrounded by South African territory. South Africa’s coastlines border the Indian Ocean to the southeast and the Atlantic Ocean to the southwest. The country possesses two small subantarctic islands, Prince Edward and Marion, situated in the Indian Ocean about 1,200 miles (1,900 km) southeast of Cape Town. The former South African possession of Walvis Bay, on the Atlantic coast some 400 miles (600 km) north of the Orange River, became part of Namibia in 1994. Relief of South Africa A plateau covers the largest part of the country, dominating the topography; it is separated from surrounding areas of generally lower elevation by the Great Escarpment. The plateau consists almost entirely of very old rock of the Karoo System, which formed from the Late Carboniferous Epoch (about 320 to 300 million years ago) to the Late Triassic Epoch (about 230 to 200 million years ago). The plateau, generally highest in the east, drops from elevations of more than 8,000 feet (2,400 metres) in the basaltic Lesotho region to about 2,000 feet (600 metres) in the sandy Kalahari in the west. The central part of the plateau comprises the Highveld, which reaches between 4,000 and 6,000 feet (1,200 and 1,800 metres) in elevation. South of the Orange River lies the Great Karoo region. The Great Escarpment (see Drakensberg), known by a variety of local names such as uKhahlamba (Zulu: “Barrier of Spears”) and the Natal Drakensberg, forms the longest continuous topographic feature in South Africa and provides scenery of great beauty. The escarpment is part of uKhahlamba/Drakensberg Park, which was designated a UNESCO World Heritage site in 2000. It runs southward from the far northeast, where it is generally known as the Transvaal Drakensberg (Afrikaans: “Dragon Mountains”). It is there, in KwaZulu-Natal province, that the country’s highest point, Njesuthi (11,181 feet [3,408 metres]), is found. Farther south the escarpment forms the boundary first between KwaZulu-Natal and Free State provinces and then between KwaZulu-Natal and Lesotho. There it reaches elevations of nearly 11,000 feet (3,300 metres), including some of the country’s highest peaks, such as Mont aux Sources (10,823 feet [3,299 metres]). The mountainous escarpment continues southwestward, dividing Lesotho from the Eastern Cape province, where it runs westward across Eastern Cape at lesser elevations of 5,000 to 8,000 feet (1,500 to 2,400 metres) and is known as the Stormberg. Farther to the west it becomes the Nuweveld Range and the Roggeveld Mountains and forms the approximate boundary between Northern Cape and Western Cape provinces. At its western extreme, in the vicinity of Mount Bokkeveld and Mount Kamies (5,600 feet [1,700 metres]), the escarpment is not well defined.An area of ancient folded mountains with elevations between 3,000 and 7,600 feet (900 and 2,300 metres) lies in the southwest of the country; it includes ranges such as the Tsitsikama, Outeniqua, Groot-Swart, Lange, Ceder, Drakenstein, and Hottentots Holland mountains, as well as Table Mountain and its associated features at Cape Town. Both above and below the Great Escarpment, the topography tends to be broken. Open plains are rare, occurring mainly in northwestern Free State and farther to the west and in smaller areas such as the Springbok Flats north of Pretoria. Ridges, mountains, and deeply incised valleys are common, mainly left by the erosion of ancient landforms. There is little genuine coastal plain between the escarpment and the sea, except in northern KwaZulu-Natal, where it reaches a width of about 50 miles (80 km), and in parts of Western Cape. For most of its 1,836-mile (2,955-km) length, the coastline consists of fairly steep slopes rising rapidly inland and often includes long stretches of beach. Most of the coastline has been uplifted or created by falling sea levels in the recent geologic past, with the result that there are few flooded river valleys or natural harbours. Exceptions include the Knysna Lagoon in Western Cape and the Buffalo River at East London. In KwaZulu-Natal, longshore drift over many centuries has created spits and bluffs from beach sand; in a number of places these features have enclosed bays, which have provided both remarkable sanctuaries for wildlife (as at the St. Lucia estuary) and, when mouths are dredged, good harbours (as at Durban and Richards Bay). More …. Score: https://www.britannica.com/place/South-Africa/Relief  

2021/04/27

Reunification Day United Republic of Tanzania

Tanzania, East African country situated just south of the Equator. Tanzania was formed as a sovereign state in 1964 through the union of the theretofore separate states of Tanganyika and Zanzibar. Mainland Tanganyika covers more than 99 percent of the combined territories’ total area. Mafia Island is administered from the mainland, while Zanzibar and Pemba islands have a separate government administration. Dodoma, since 1974 the designated official capital of Tanzania, is centrally located on the mainland. Dar es Salaam is the largest city and port in the country. Land - Tanzania mainland The Tanzania mainland is bounded by Uganda, Lake Victoria, and Kenya to the north, by the Indian Ocean to the east, by Mozambique, Lake Nyasa, Malawi, and Zambia to the south and southwest, and by Lake Tanganyika, Burundi, and Rwanda to the west. Relief Except for the narrow coastal belt of the mainland and the offshore islands, most of mainland Tanzania lies above 600 feet (200 metres) in elevation. Vast stretches of plains and plateaus contrast with spectacular relief features, notably Africa’s highest mountain, Kilimanjaro (19,340 feet [5,895 metres]), and the world’s second deepest lake, Lake Tanganyika (4,710 feet [1,436 metres] deep). Highlands associated with the Western Rift Valley are formed by the Ufipa Plateau, the Mbeya Range, and Rungwe Mountain in the southwestern corner of the country. From there the southern highlands run northeastward along the Great Rift to the Ukuguru and Nguru mountains northwest of Morogoro. Extending from the northern coast, the Usambara and Pare mountain chains run in a southeast-to-northwest direction, culminating in Kilimanjaro’s lofty snow-clad peak and continuing beyond to Mount Meru (14,978 feet [4,565 metres]). Immediately to the west of Mount Meru, another chain of mountains begins, which includes the still-active volcano Ol Doinyo Lengai and the Ngorongoro Crater, the world’s largest caldera, or volcanic depression. This chain extends through a corridor between Lake Eyasi and Lake Manyara toward Dodoma. Drainage Because of its numerous lakes, approximately 22,800 square miles (59,000 square km) of Tanzania’s territory consists of inland water. Lake Victoria, which ranks as the world’s second largest freshwater lake, is not part of the Rift System. Although Tanzania has no big rivers, it forms the divide from which the three great rivers of the African continent rise—the Nile, the Congo, and the Zambezi, which flow to the Mediterranean Sea, the Atlantic Ocean, and the Indian Ocean, respectively. Separated by the central plateau, the watersheds of these rivers do not meet. All of Tanzania’s major rivers—the Ruvuma, the Rufiji, the Wami, and the Pangani—drain into the Indian Ocean. The largest, the Rufiji River, has a drainage system that extends over most of southern mainland Tanzania. The Kagera River flows into Lake Victoria, whereas other minor rivers flow into internal basins formed by the Great Rift Valley. With so many rivers, mainland Tanzania is rich in hydroelectricity potential. Soils The variety of soils in mainland Tanzania surpasses that of any other country in Africa. The reddish brown soils of volcanic origin in the highland areas are the most fertile. Many river basins also have fertile soils, but they are subject to flooding and require drainage control. The red and yellow tropical loams of the interior plateaus, on the other hand, are of moderate-to-poor fertility. In these regions, high temperatures and low rainfall encourage rapid rates of oxidation, which result in a low humus content in the soil and, consequently, a clayey texture rather than the desired crumblike structure of temperate soils. Also, tropical downpours, often short in duration but very intense, compact the soil; this causes drainage problems and leaches the soil of nutrients. Climate Mainland Tanzania can be divided into four principal climactic and topographic areas: the hot and humid coastal lowlands of the Indian Ocean shoreline, the hot and arid zone of the broad central plateau, the high inland mountain and lake region of the northern border, where Mount Kilimanjaro is situated, and the highlands of the northeast and southwest, the climates of which range from tropical to temperate. Tanzania’s warm equatorial climate is modified by variations in elevation. The high amount of solar radiation throughout the year is associated with a limited seasonal fluctuation of temperature: the mean monthly variation is less than 9 °F (5 °C) at most stations. Ground frosts rarely occur below 8,200 feet (2,500 metres). Rainfall is highly seasonal, being influenced greatly by the annual migration of the intertropical convergence zone. Roughly half of mainland Tanzania receives less than 30 inches (750 mm) of precipitation annually, an amount considered to be the minimum required for most forms of crop cultivation in the tropics. The central plateau, which receives less than 20 inches (510 mm) per year on average, is the driest area and experiences a single rainy season between December and May. Precipitation is heavier on the coast, where there are two peaks of precipitation: October–November and April–May. The offshore islands and many highland areas have high annual precipitation totals of more than 60 inches (1,520 mm). More …. Score: www.britannica.com/place/Tanzania

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