Republic of Korea Day of the Establishment of the Korean State

South Korea, country in East Asia. It occupies the southern portion of the Korean peninsula. The country is bordered by the Democratic People’s Republic of Korea (North Korea) to the north, the East Sea (Sea of Japan) to the east, the East China Sea to the south, and the Yellow Sea to the west; to the southeast it is separated from the Japanese island of Tsushima by the Korea Strait. South Korea makes up about 45 percent of the peninsula’s land area. The capital is Seoul (Sŏul). South Korea faces North Korea across a demilitarized zone (DMZ) 2.5 miles (4 km) wide that was established by the terms of the 1953 armistice that ended fighting in the Korean War (1950–53). The DMZ, which runs for about 150 miles (240 km), constitutes the 1953 military cease-fire line and roughly follows latitude 38° N (the 38th parallel) from the mouth of the Han River on the west coast of the Korean peninsula to a little south of the North Korean town of Kosŏng on the east coast. Land - Relief Geologically, South Korea consists in large part of Precambrian rocks (i.e., more than about 540 million years old) such as granite and gneiss. The country is largely mountainous, with small valleys and narrow coastal plains. The T’aebaek Mountains run in roughly a north-south direction along the eastern coastline and northward into North Korea, forming the country’s drainage divide. From them several mountain ranges branch off with a northeast-southwest orientation. The most important of these are the Sobaek Mountains, which undulate in a long S-shape across the peninsula. None of South Korea’s mountains are very high: the T’aebaek Mountains reach an elevation of 5,604 feet (1,708 metres) at Mount Sŏrak in the northeast, and the Sobaek Mountains reach 6,283 feet (1,915 metres) at Mount Chiri. The highest peak in South Korea, the extinct volcano Mount Halla on Cheju Island, is 6,398 feet (1,950 metres) above sea level. South Korea has two volcanic islands—Cheju (Jeju), off the peninsula’s southern tip, and Ullŭng, about 85 miles (140 km) east of the mainland in the East Sea—and a small-scale lava plateau in Kangwŏn province. In addition, South Korea claims and occupies a group of rocky islets—known variously as Liancourt Rocks, Tok (Dok) Islands (Korean), and Take Islands (Japanese)—some 55 miles (85 km) southeast of Ullŭng Island; these islets also have been claimed by Japan. There are fairly extensive lowlands along the lower parts of the country’s main rivers. The eastern coastline is relatively straight, whereas the western and southern have extremely complicated ria (i.e., creek-indented) coastlines with many islands. The shallow Yellow Sea and the complex Korean coastline produce one of the most pronounced tidal variations in the world—about 30 feet (9 metres) maximum at Inch’ŏn (Incheon), the entry port for Seoul. Drainage South Korea’s three principal rivers, the Han, Kŭm, and Naktong, all have their sources in the T’aebaek Mountains, and they flow between the ranges before entering their lowland plains. Nearly all the country’s rivers flow westward or southward into either the Yellow Sea or the East China Sea; only a few short, swift rivers drain eastward from the T’aebaek Mountains. The Naktong River, South Korea’s longest, runs southward for 325 miles (523 km) to the Korea Strait. Streamflow is highly variable, being greatest during the wet summer months and considerably less in the relatively dry winter. Soils Most of South Korea’s soils derive from granite and gneiss. Sandy and brown-coloured soils are common, and they are generally well-leached and have little humus content. Podzolic soils (ash-gray forest soils), resulting from the cold of the long winter season, are found in the highlands. Climate The greatest influence on the climate of the Korean peninsula is its proximity to the main Asian landmass. This produces the marked summer-winter temperature extremes of a continental climate while also establishing the northeast Asian monsoons (seasonal winds) that affect precipitation patterns. The annual range of temperature is greater in the north and in interior regions of the peninsula than in the south and along the coast, reflecting the relative decline in continental influences in the latter areas. South Korea’s climate is characterized by a cold, relatively dry winter and a hot, humid summer. The coldest average monthly temperatures in winter drop below freezing except along the southern coast. The average January temperature at Seoul is in the low 20s °F (about −5 °C), while the corresponding average at Pusan (Busan), on the southeast coast, is in the mid-30s °F (about 2 °C). By contrast, summer temperatures are relatively uniform across the country, the average monthly temperature for August (the warmest month) being in the high 70s °F (about 25 °C). Annual precipitation ranges from about 35 to 60 inches (900 to 1,500 mm) on the mainland. Taegu, on the east coast, is the driest area, while the southern coast is the wettest; southern Cheju Island receives more than 70 inches (1,800 mm) annually. Up to three-fifths of the annual precipitation is received in June–August, during the summer monsoon, the annual distribution being more even in the extreme south. Occasionally, late-summer typhoons (tropical cyclones) cause heavy showers and storms along the southern coast. Precipitation in winter falls mainly as snow, with the heaviest amounts occurring in the T’aebaek Mountains. The frost-free season ranges from 170 days in the northern highlands to more than 240 days on Cheju Island. Plant and animal life The long, hot, humid summer is favourable for the development of extensive and varied vegetation. Some 4,500 plant species are known. Forests once covered about two-thirds of the total land area, but, because of fuel needs during the long, cold winter and the country’s high population density, the original forest has almost disappeared. Except for evergreen broad-leaved forests in the narrow subtropical belt along the southern coast and on Cheju Island, most areas contain deciduous broad-leaved and coniferous trees. Typical evergreen broad-leaved species include camellias and camphor trees, while deciduous forests include oaks, maples, alders, zelkovas, and birches. Species of pine are the most representative in the country; other conifers include spruces, larches, and yews. Among indigenous species are the Abeliophyllum distichum (white forsythia or Korean abelia), a shrub of the olive family, and the Korean fir (Abies koreana). Wild animal life is similar to that of northern and northeastern China. The most numerous larger mammals are deer. Tigers, leopards, lynx, and bears, formerly abundant, have almost disappeared, even in remote areas. Some 380 species of birds are found in the country, most of which are seasonal migrants. Many of South Korea’s fish, reptile, and amphibian species are threatened by intensive cultivation and environmental pollution except in the DMZ between North and South Korea, which has become a de facto nature preserve. Once farmland, and subsequently a devastated battleground, the DMZ has lain almost untouched since the end of hostilities and has reverted to nature to a large extent, making it one of the most pristine undeveloped areas in Asia. It contains many ecosystems including forests, estuaries, and wetlands frequented by migratory birds. The zone serves as a sanctuary for hundreds of bird species, among them the endangered white-naped and red-crowned cranes, and is home to dozens of fish species and Asiatic black bears, lynxes, and other mammals. More … Score https://www.britannica.com/place/South-Korea  

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Republic of Guinea Proclamation of the Republic

Guinea, country of western Africa, located on the Atlantic coast. Three of western Africa’s major rivers—the Gambia, the Niger, and the Sénégal—rise in Guinea. Natural resources are plentiful: in addition to its hydroelectric potential, Guinea possesses a large portion of the world’s bauxite reserves and significant amounts of iron, gold, and diamonds. Nonetheless, the economy is largely based on subsistence agriculture. Guinea, under the name French Guinea, was a part of French West Africa until it achieved independence in 1958. It then was ruled successively by Sékou Touré (1958–84) and Lansana Conté (1984–2008), the latter of whom claimed power through a military coup. During the 1990s Guinea accommodated several hundred thousand war refugees from neighbouring Liberia and Sierra Leone, and conflicts between those countries and Guinea have continued to flare up over the refugee population. Following Conté’s death, a military junta took control of the country and suspended the constitution that had been adopted in 1991. Power was handed over to a freely elected civilian administration in 2010. The national capital, Conakry, lies on Tombo (Tumbo) Island and spreads up the Camayenne (Kaloum) Peninsula; it is the country’s main port. Land Guinea is bordered by Guinea-Bissau to the northwest, Senegal to the north, Mali to the northeast, Côte d’Ivoire to the southeast, and Liberia and Sierra Leone to the south. The Atlantic Ocean lies to the west. , Inc. Guinea consists of four geographic regions: Lower Guinea, the Fouta Djallon, Upper Guinea, and the Forest Region, or Guinea Highlands. Lower Guinea includes the coast and coastal plain. The coast has undergone recent marine submergence and is marked by rias, or drowned river valleys, that form inlets and tidal estuaries. Numerous offshore islands are remnants of former hills. Immediately inland the gently rolling coastal plain rises to the east, being broken by rocky spurs of the Fouta Djallon highlands in the north at Cape Verga and in the south at the Camayenne Peninsula. Between 30 and 50 miles (48 and 80 km) wide, the plain is wider in the south than the north. Its base rocks of granite and gneiss (coarse-grained rock containing bands of minerals) are covered with laterite (red soil with a high content of iron oxides and aluminum hydroxide) and sandstone gravel. The Fouta Djallon highlands rise sharply from the coastal plain in a series of abrupt faults. More than 5,000 square miles (13,000 square km) of the highlands’ total extent of 30,000 square miles (78,000 square km) lie above 3,000 feet (900 metres). Basically an enormous sandstone block, the Fouta Djallon consists of level plateaus broken by deeply incised valleys and dotted with sills and dikes, or exposed structures of ancient volcanism resulting in resistant landforms of igneous rock. The Kakoulima Massif, for example, attains 3,273 feet (998 metres) northeast of Conakry. The highest point in the highlands, Mount Tamgué, rises to 5,046 feet (1,538 metres) near the town of Mali in the north. Upper Guinea is composed of the Niger Plains, which slope northeastward toward the Sahara. The flat relief is broken by rounded granite hills and outliers of the Fouta Djallon. Composed of granite, gneiss, schist (crystalline rock), and quartzite, the region has an average elevation of about 1,000 feet (300 metres). The Forest Region, or Guinea Highlands, is a historically isolated area of hills in the country’s southeastern corner. Mount Nimba (5,748 feet [1,752 metres]), the highest mountain in the region, is located at the borders of Guinea, Liberia, and Côte d’Ivoire. The mountain’s densely forested slopes are part of the Mount Nimba Strict Nature Reserve, which has significant portions in Guinea. The Guinean sector was designated a UNESCO World Heritage site in 1981 and is home to a unique and diverse array of flora and fauna. The rocks of this region are of the same composition as those of Upper Guinea. Drainage and soils More than 20 rivers in western Africa originate in Guinea. The Fouta Djallon is the source of the three major rivers of the region. The Niger River and several tributaries, including the Tinkisso, Milo, and Sankarani, rise in the highlands and flow in a general northeasterly direction across Upper Guinea to Mali. The Bafing and Bakoye rivers, headwaters of the Sénégal River, flow northward into Mali before uniting to form the main river. The Gambia River flows northwestward before crossing Senegal and The Gambia. The Fouta Djallon also gives rise to numerous smaller rivers, including the Fatala, Konkouré, and Kolenté, which flow westward across the coastal plain to enter the Atlantic Ocean. The Forest Region generally drains to the southwest through Sierra Leone and Liberia. The Saint Paul River enters the Atlantic at Monrovia, in Liberia, and the Moa River has its mouth at Sulima, in Sierra Leone. The most common soils found in Guinea are laterites formed of iron and hydrated aluminum oxides and other materials that often concretize into hard iron-rich conglomerates. Sandy brown soils predominate in the northeast, while black, heavy clay soils accumulate in the backwaters along the coast. There are alluvial soils along the major rivers. Soil conservation is extremely important, because most soils are thin and rainfall heavy, causing much erosion. Climate The climate of Guinea is tropical with two alternating seasons—a dry season (November through March) and a wet season (April through October). The arrival of the migratory intertropical convergence zone (ITCZ) in June brings the heaviest rainfall of the wet season. As the ITCZ shifts southward in November, the hot, dry wind known as the harmattan blows from the northeast off the Sahara. On the coast a period of six months of dry weather is followed by six months of rain. The average rainfall at Conakry is about 170 inches (4,300 mm) a year, and the average annual temperatures are in the low 80s F (about 27 °C). In the Fouta Djallon, January afternoon temperatures range from the mid-80s to the mid-90s F (about 30 to 35 °C), while evening temperatures dip into the high 40s and low 50s F (about 8 to 11 °C). Rainfall varies between 60 and 90 inches (1,500 and 2,300 mm) annually, and the average annual temperatures there are in the mid-70s F (about 25 °C). In Upper Guinea rainfall drops to about 60 inches (1,500 mm) a year. During the dry season temperatures of more than 100 °F (38 °C) are common in the northeast. In the Forest Region at Macenta there may be some 100 or more inches (2,540 mm) of rain annually. Only the months of December, January, and February are relatively dry, with possible rainfall of only 1 inch (25 mm). At low elevations, temperatures resemble those of the coastal areas. Plant and animal life The coast is fringed with mangrove trees, and the coastal plain supports stands of oil palms. The Fouta Djallon is mostly open, with trees growing along the wider stream valleys. Badiar National Park, which is administered jointly with Niokolo-Koba National Park in southeastern Senegal, contains savanna and forest. In Upper Guinea the savanna grassland supports several species of tall grasses that reach heights of 5 to 10 feet (1.5 to 3 metres) during the rainy season. Deciduous trees grow in scattered clumps, but few have commercial value; baobabs and shea trees furnish fruit and oil. Many of the dry woodlands of the region are protected in Haut Niger National Park, located in the centre of the country. The Forest Region contains several extensive patches of rainforest, with teak, mahogany, and ebony trees; agriculture, however, has diminished the forests and resulted in a shift largely toward open savanna. Guinea is not rich in African big game. Baboons and hyenas are common, while an occasional wild boar, several types of antelope, and a rare leopard may be sighted. A few hippopotamuses and manatees inhabit the rivers of both Lower and Upper Guinea. Monkeys, chimpanzees, and some rare bird species can be found in the southern portion of the Forest Region, near the Liberian border. Poisonous snakes include mambas, vipers, and cobras, and there are pythons and a variety of harmless snakes. Crocodiles and several varieties of fish are found in most rivers. More … Score: https://www.britannica.com/place/Guinea

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Botswana Tourism Organisation: Home

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