National Day of the Republic of Iraq

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Day of German Unity of the Federal Republic of Germany

Germany, officially Federal Republic of Germany, German Deutschland or Bundesrepublik Deutschland, country of north-central Europe, traversing the continent’s main physical divisions, from the outer ranges of the Alps northward across the varied landscape of the Central German Uplands and then across the North German Plain. One of Europe’s largest countries, Germany encompasses a wide variety of landscapes: the tall, sheer mountains of the south; the sandy, rolling plains of the north; the forested hills of the urbanized west; and the plains of the agricultural east. At the spiritual heart of the country is the magnificent east-central city of Berlin, which rose phoenixlike from the ashes of World War II and now, after decades of partition, is the capital of a reunified Germany, and the Rhine River, which flows northward from Switzerland and is celebrated in visual art, literature, folklore, and song. Along its banks and those of its principal tributaries—among them the Neckar, Main, Moselle, and Ruhr—stand hundreds of medieval castles, churches, picturesque villages, market towns, and centres of learning and culture, including Heidelberg, the site of one of Europe’s oldest universities (founded in 1386), and Mainz, historically one of Europe’s most important publishing centres. All are centrepieces of Germany’s thriving tourist economy, which brings millions of visitors to the country each year, drawn by its natural beauty, history, culture, and cuisine (including its renowned wines and beers). The name Germany has long described not a particular place but the loose, fluid polity of Germanic-speaking peoples that held sway over much of western Europe north of the Alps for millennia. Although Germany in that sense is an ancient entity, the German nation in more or less its present form came into being only in the 19th century, when Prussian Prime Minister Otto von Bismarck brought together dozens of German-speaking kingdoms, principalities, free cities, bishoprics, and duchies to form the German Empire in 1871. This so-called Second Reich quickly became Europe’s leading power and acquired colonies in Africa, Asia, and the Pacific. That overseas empire was dismantled following Germany’s defeat in World War I and the abdication of Emperor William II. Economic depression, widespread unemployment, and political strife that verged on civil war followed, leading to the collapse of the progressive Weimar Republic and the rise of the Nazi Party under Adolf Hitler. After gaining power in 1933, Hitler established the Third Reich and soon thereafter embarked on a ruinous crusade to conquer Europe and exterminate Jews, Roma (Gypsies), homosexuals, and others. The Third Reich disintegrated in 1945, brought down by the Allied armies of the United States, the United Kingdom, the Soviet Union, France, and other countries. The victorious powers divided Germany into four zones of occupation and later into two countries: the Federal Republic of Germany (West Germany) and the German Democratic Republic (East Germany), separated for more than 40 years by a long boundary. In East Germany this boundary was, until the fall of its communist government in 1989, marked by defenses designed to prevent escape. The 185 square miles (480 square km) of the “island” of West Berlin were similarly ringed from 1961 to 1989 by the Berlin Wall running through the city and by a heavily guarded wire-mesh fence in the areas abutting the East German countryside. Although Berlin was a flashpoint between the United States and the Soviet Union during the Cold War, the city declined in national and international significance until 1989–90, when a popular and peaceful uprising toppled the East German government and soon after restored a united Berlin as the capital of a reunified Germany. Since World War II, Germany has made great efforts to both commemorate the victims and redress the crimes of the Holocaust, providing strong material and political support for the state of Israel and actively prosecuting hate crimes and the propagation of neo-Nazi doctrine; the latter became an issue in the 1990s with the rise in Germany of anti-immigrant skinhead groups and the availability of Hitler’s Mein Kampf over the Internet. Clearly, modern Germany struggles to balance its national interests with those of an influx of political and economic refugees from far afield, especially North Africa, Turkey, and South Asia, an influx that has fueled ethnic tensions and swelled the ranks of nationalist political parties, particularly in eastern Germany, where unemployment was double that of the west. Tensions became especially acute in the second decade of the 21st century, when more than one million migrants entered Germany in the wake of the revolutions of the Arab Spring and the Syrian Civil War. The constitution of the republic, adopted in 1949 by West Germany, created a federal system that gives significant government powers to its constituent Länder (states). Before unification there were 11 West German Länder (including West Berlin, which had the special status of a Land without voting rights), but, with the accession of East Germany, there are now 16 Länder in the unified republic. The largest of the states is Bavaria (Bayern), the richest is Baden-Württemberg, and the most populous is North Rhine–Westphalia (Nordrhein-Westfalen). Matters of national importance, such as defense and foreign affairs, are reserved to the federal government. At both the state and federal levels, parliamentary democracy prevails. The Federal Republic has been a member of the North Atlantic Treaty Organization (NATO) since 1955 and was a founding member of the European Economic Community (see European Union). During the four decades of partition, the Federal Republic concluded a number of agreements with the Soviet Union and East Germany, which it supported to some extent economically in return for various concessions with regard to humanitarian matters and access to Berlin. West Germany’s rapid economic recovery in the 1950s (Wirtschaftswunder, or “economic miracle”) brought it into a leading position among the world’s economic powers, a position that it has maintained. Much of Germany’s post-World War II success has been the result of the renowned industriousness and self-sacrifice of its people, about which novelist Günter Grass, winner of the Nobel Prize for Literature in 1999, remarked, “To be a German is to make the impossible possible.” He added, more critically, For in our country everything is geared to growth. We’re never satisfied. For us enough is never enough. We always want more. If it’s on paper, we convert it into reality. Even in our dreams we’re productive. This devotion to hard work has combined with a public demeanour—which is at once reserved and assertive—to produce a stereotype of the German people as aloof and distant. Yet Germans prize both their private friendships and their friendly relations with neighbours and visitors, place a high value on leisure and culture, and enjoy the benefits of life in a liberal democracy that has become ever more integrated with and central to a united Europe. Land of Germany Germany is bounded at its extreme north on the Jutland peninsula by Denmark. East and west of the peninsula, the Baltic Sea (Ostsee) and North Sea coasts, respectively, complete the northern border. To the west, Germany borders The Netherlands, Belgium, and Luxembourg; to the southwest it borders France. Germany shares its entire southern boundary with Switzerland and Austria. In the southeast the border with the Czech Republic corresponds to an earlier boundary of 1918, renewed by treaty in 1945. The easternmost frontier adjoins Poland along the northward course of the Neisse River and subsequently the Oder to the Baltic Sea, with a westward deviation in the north to exclude the former German port city of Stettin (now Szczecin, Poland) and the Oder mouth. This border reflects the loss of Germany’s eastern territories to Poland, agreed to at the Yalta Conference (February 1945), mandated at the Potsdam Conference (July–August 1945) held among the victorious World War II Allies, and reaffirmed by subsequent governments. The major lineaments of Germany’s physical geography are not unique. The country spans the great east-west morphological zones that are characteristic of the western part of central Europe. In the south Germany impinges on the outermost ranges of the Alps. From there it extends across the Alpine Foreland (Alpenvorland), the plain on the northern edge of the Alps. Forming the core of the country is the large zone of the Central German Uplands, which is part of a wider European arc of territory stretching from the Massif Central of France in the west into the Czech Republic, Slovakia, and Poland in the east. In Germany it manifests itself as a landscape with a complex mixture of forested block mountains, intermediate plateaus with scarped edges, and lowland basins. In the northern part of the country the North German Plain, or Lowland, forms part of the greater North European Plain, which broadens from the Low Countries eastward across Germany and Poland into Belarus, the Baltic states, and Russia and extends northward through Schleswig-Holstein into the Jutland peninsula of Denmark. The North German Plain is fringed by marshes, mudflats, and the islands of the North and Baltic seas. In general, Germany has a south-to-north drop in altitude, from a maximum elevation of 9,718 feet (2,962 metres) in the Zugspitze of the Bavarian Alps to a few small areas slightly below sea level in the north near the coast. It is a common assumption that surface configuration reflects the underlying rock type; a hard resistant rock such as granite will stand out, whereas a softer rock such as clay will be weathered away. However, this assumption is not always borne out. The Zugspitze, for example, is Germany’s highest summit not because it is composed of particularly resistant rocks but because it was raised by the mighty earth movements that began some 37 to 24 million years ago and created the Alps, Europe’s highest and youngest fold mountains. Another powerful force determining surface configuration is erosion, mainly by rivers. In the Permian Period (some 290 million years ago) an earlier mountain chain—the Hercynian, or Variscan, mountains—had crossed Europe in the area of the Central German Uplands. Yet the forces of erosion were sufficient to reduce these mountains to almost level surfaces, on which a series of secondary sedimentary rocks of Permian to Jurassic age (about 300 to 145 million years old) were deposited. The entire formation was subsequently fractured and warped under the impact of the Alpine orogeny. This process was accompanied by some volcanic activity, which left behind not only peaks but also a substantial number of hot and mineral springs. Dramatic erosion occurred as the Alpine chains were rising, filling the furrow that now constitutes the Alpine Foreland. The pattern of valleys eroded by streams and rivers has largely given rise to the details of the present landscape. Valley glaciers emerging from the Alps and ice sheets from Scandinavia had some erosive effect, but they mainly contributed sheets of glacial deposits. Slopes outside the area of the actual ice sheets—those under tundra conditions and unprotected by vegetation—were rendered less steep by the periglacial slumping of surface deposits under the influence of gravitation. Winds blowing over unprotected surfaces fringing the ice sheets picked up fine material known as loess; once deposited, it became Germany’s most fertile soil-parent material. Coarser weathered material was carried into alluvial cones and gravel-covered river terraces, as in the Rhine Rift Valley (Rhine Graben). The detailed morphology of Germany is significant in providing local modifications to climate, hydrology, and soils, with consequent effects on vegetation and agricultural utilization. More … Score:

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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  

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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:

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Tuvalu Independence Day

Tuvalu, formerly Ellice Islands, country in the west-central Pacific Ocean. It is composed of nine small coral islands scattered in a chain lying approximately northwest to southeast over a distance of some 420 miles (676 km). The de facto capital is the village of Vaiaku, where most government offices are located. It is on Fongafale islet, a constituent part of Funafuti Atoll. Together with what is now Kiribati (formerly the Gilbert Islands), Tuvalu formed the British Gilbert and Ellice Islands Colony before separately gaining its independence in 1978. Land The group includes both atolls and reef islands. The atolls—Nanumea, Nui, Nukufetau, Funafuti, and Nukulaelae—have islets encircling a shallow lagoon; the reef islands—Nanumanga, Niutao, Vaitupu, and Niulakita—are compact with a fringing reef. The islands are low-lying, most being 13 to 16 feet (4 to 5 metres) above sea level. There are no rivers; rain catchment and wells provide the only fresh water. Rainfall averages 100 inches (2,500 mm) in the north and 125 inches (3,175 mm) in the south. The prevailing winds are southeast trades; westerly storms occur from November to February. Daytime temperatures range from 80 to 85 °F (27 to 29 °C). Because the soils are porous, agriculture is limited. Coconut palms thrive, and breadfruit trees, pandanus, taro, and bananas are grown. Pigs and chickens are raised, and seabirds, fish, and shellfish are caught for food. The islands increasingly depend on imported food. People The Tuvaluans are Polynesian, and their language, Tuvaluan, is closely related to Samoan. Nui, however, was heavily settled in prehistoric times by Micronesians from the Gilbert Islands (now Kiribati). English is taught in the schools and widely used. The vast majority of the population belongs to the Church of Tuvalu (the former Ellice Islands Protestant Church). Although most people live on the outer islands in extended family households clustered into villages, about one-third of the population lives on Funafuti, the centre of government and commerce. Population growth has been slowed by family planning; life expectancy at birth is about 60 years. About 10 percent of the population lives overseas, either pursuing education, working in the Nauru phosphate industry, or working on merchant ships. Economy Most Tuvaluans are subsistence farmers and are aided by remittances from relatives working overseas. A small quantity of copra is produced for export, the sale of stamps accounts for modest earnings, and fees are collected from foreign fishing fleets, but the country depends heavily on foreign aid. It imports most of its food, fuel, and manufactured goods. Fiji, Australia, New Zealand, and Japan are among the country’s major trade partners. Retailing is handled by community-based cooperative societies. Tuvalu uses Australian currency but also issues its own coinage. There is a single bank, a joint government-commercial venture. Tuvalu has air links with Kiribati and Fiji; for international shipping, it depends on irregular regional services. Seaplanes have been used for interisland travel, but generally the outer islands depend on a single government vessel. Motorcycles are common on Funafuti, but there are few automobiles. Government and society Tuvalu is a constitutional monarchy within the Commonwealth, with the British monarch (through a governor-general) as head of state. The government is a parliamentary democracy with a unicameral legislature elected by universal adult suffrage. There are no political parties: the prime minister is chosen by and from the legislature. Tuvalu is a member of the South Pacific Forum. The government provides universal primary education and, under a joint arrangement with the Church of Tuvalu, secondary education to school certificate level for selected pupils. A few are sent overseas for further education and training. Medical facilities are centralized on Funafuti, but all other islands have clinics with trained medical staff. Cultural life The Tuvaluan lifestyle has been Westernized to an extent, but Western-style amenities are few. Only Funafuti has a regular electricity supply; the government publishes a brief news sheet, but there is no newspaper; a few motion pictures are shown; satellite television service is available only by subscription; and there is only a single radio station. Most Tuvaluans live in villages of a few hundred people, tend their gardens, and fish from handcrafted canoes. Traditional music and dancing still enjoy a strong following, along with Western forms. Volleyball, football (soccer), and cricket are popular. Tuvaluan life, despite modernization, still rests on a firm traditional base that emphasizes the importance of community consensus and identity. History of Tuvalu The first settlers were from Samoa and probably arrived in the 14th century ad. Smaller numbers subsequently arrived from Tonga, the northern Cook Islands, Rotuma, and the Gilbert Islands. Niulakita, the smallest and southernmost island, was uninhabited before European contact; the other islands were settled by the 18th century, giving rise to the name Tuvalu, or “Cluster of Eight.” Europeans first discovered the islands in the 16th century through the voyages of Álvaro de Mendaña de Neira, but it was only from the 1820s, with visits by whalers and traders, that they were reliably placed on European charts. In 1863 labour recruiters from Peru kidnapped some 400 people, mostly from Nukulaelae and Funafuti, reducing the population of the group to less than 2,500. A few were later recruited for plantations in Queensland, Australia, as well as in Fiji, Samoa, and Hawaii. Concern over labour recruiting and a desire for protection helps to explain the enthusiastic response to Samoan pastors of the London Missionary Society who arrived in the 1860s. By 1900, Protestant Christianity was firmly established. With imperial expansion the group, then known as the Ellice Islands, became a British protectorate in 1892 and part of the Gilbert and Ellice Islands Colony in 1916. There was a gradual expansion of government services, but most administration was through island governments supervised by a single district officer based in Funafuti. Ellice Islanders sought education and employment at the colonial capital in the Gilbert group or in the phosphate industry at Banaba or Nauru. During World War II, U.S. forces were based on Nanumea, Nukufetau, and Funafuti, but hostilities did not reach the group. From the 1960s, racial tension and rivalries over employment emerged between Gilbertese and Ellice Islanders. Ellice Islanders’ demands for secession resulted in a referendum in 1974, transition to separate colonial status between October 1975 and January 1976, and independence as Tuvalu in 1978. After independence the main priorities were to establish the infrastructure for a separate, if small, nation, and to seek foreign assistance to match political independence with economic viability. More … Score:  

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Independence day of the Republic of Palau

Palau, country in the western Pacific Ocean. It consists of some 340 coral and volcanic islands perched on the Kyushu-Palau Ridge. The Palau (also spelled Belau or Pelew) archipelago lies in the southwest corner of Micronesia, with Guam 830 miles (1,330 km) to the northeast, New Guinea 400 miles (650 km) to the south, and the Philippines 550 miles (890 km) to the west, A huge barrier reef system, continuous on the west and broken on the east, encircles most of the archipelago. Its major populated islands are Babelthuap (Babeldaob), Koror, Malakal, Arakabesan, and Peleliu. The sparsely populated Kayangel Islands to the north of Babelthuap and the raised coral islands of Angaur, Sonsorol, Pulo Anna, and Tobi south of Peleliu lie outside the barrier reef system. Palau was a member of the UN Trust Territory of the Pacific Islands, which was established in 1947 and administered by the United States. The U.S. government dissolved the trusteeship in 1986, but repeated measures to win the required support for a compact of free association between Palau and the United States were unsuccessful until 1993. The Republic of Palau officially became a sovereign state on October 1, 1994. Koror island, rising to 2,061 feet (628 metres) just south of Babelthuap, is home to Koror city, the largest population centre and former capital. Melekeok, on Babelthuap, became the capital in October 2006. The site in Melekeok where the country’s capitol complex is located is called Ngerulmud. Land - Relief and drainage All but six of Palau’s islands lie within an expansive lagoon, enclosed by the barrier reef, that stretches northeast to southwest for almost 70 miles (115 km). Babelthuap, the largest island (153 square miles [396 square km]), is volcanic, mainly composed of andesite, and is bounded by thick mangrove forests broken occasionally by sandy beaches on the east coast. Its highest point, Ngerchelchuus, in the northwest, is 794 feet (242 metres) high. Babelthuap is essentially a rolling upland, part grassland and part jungle, that has been incised by stream action to form a well-developed drainage system of three rivers. With about 150 inches (3,800 mm) of rain annually, considerable erosion has taken place on Babelthuap in spite of the stability provided by laterite soils, clays, and vegetation. The Palauan practice of burning the grassy upland areas during the dry season has contributed to erosion. A steel bridge connects the islands of Babelthuap and Koror. Koror in turn is linked by causeway to Malakal Island, the site of Palau’s deepwater port, and to Arakabesan Island. The combined area of the three smaller linked islands is 7 square miles (18 square km). All are of volcanic origin. However, beginning adjacent to southern Babelthuap and eastern Koror and filling the huge lagoon for 28 miles (45 km) south to Peleliu are more than 300 verdant “rock islands.” These are uplifted reef structures of coralline limestone, each deeply undercut at sea level. Some of the rock islands are large, towering some 600 feet (180 metres); these can have interior brackish lakes, containing unique organisms, that are connected to the lagoon by subterranean channels. Plant growth is thick on the rock islands and, together with the chemical action of heavy rains, has sculpted and broken their surfaces, producing razor-sharp edges and points and broken rubble. The limestone islands have rich deposits of phosphate, and the more accessible ones have been mined. The inhabited coral islands outside Palau’s reef-lagoon-island system sit on volcanic substructures and consist of the Kayangel Islands, 25 miles (40 km) north of Babelthuap, and Angaur, 6 miles (10 km) south of Peleliu. Angaur was heavily mined for its phosphate first by the Germans and later by the Japanese. Sonsorol, Pulo Anna, and Tobi, all with areas of less than 1 square mile (2.6 square km), are 180 miles (290 km) southwest of the Palau archipelago. All are flat platform structures with fringing reefs. Climate of Palau Palau’s climate is tropical. Rainfall varies from about 120 to 160 inches (3,050 to 4,060 mm) per year. Humidity is fairly constant, ranging from 77 to 84 percent, and temperatures vary not more than 10 °F (5.5 °C) diurnally, monthly, or annually from a mean in the low 80s °F (28 °C). Northeast trade winds prevail from December to March, and the southwest monsoon from June to October. Prevailing oceanic currents offshore are the North Equatorial Current and the Pacific Equatorial Countercurrent. Geologically, Palau sits on the Philippine Sea Plate only 30 miles (48 km) west of the 26,200-foot- (7,990-metre-) deep Palau Trench, the western boundary of the upthrusting Pacific Plate. Despite its close proximity to this subduction zone, Palau rarely experiences earthquake activity. Plant and animal life Palau’s marine environment exhibits a rich fauna balanced by an abundant terrestrial flora. This richness derives from Palau’s close proximity to Indonesia, New Guinea, and the Philippines. Palau has more species of marine life than any other area of similar size in the world; corals, fish, snails, clams, sea cucumbers, starfish, sea urchins, sea anemones, jellyfish, squid, and feather-duster worms exist in profusion and variety. Such marine life has made Palau one of the world’s premier scuba-diving locations. Common flora are the beach morning glory, Polynesian ironwood tree, pandanus, and various species of palm and fern. The birds of Palau are abundant and colourful, and many migrate to or through Palau twice annually. A few species of reptiles and amphibians live in Palau, including a unique frog that gives birth to live young. Insects are also abundant. The accidentally introduced coconut rhinoceros beetle can do enormous damage to coconut palms, but various biological methods are used to control its spread. People - Ethnic groups and languages The islands were inhabited from 3,000 to 2,000 years ago by successive waves of Malays from Indonesia, Melanesians from New Guinea, Philippine natives, and some Polynesians from outlying Polynesian islands in Micronesia. This resulted in a diverse population, which since the late 18th century has also included Europeans, Japanese, and Americans. The southwest islanders, who are culturally and linguistically distinct from the Palauans, are the only minority group; they trace their origin to a group of ancestral survivors of one or more canoes that drifted to Sonsorol from Ulithi Atoll, northeast of Yap. Palauan is a Western Austronesian language and is very complex in that it has many irregularities that make formulation of grammatical and lexical rules difficult. Sonsorolese-Tobian, another native language, is spoken on the southwest islands. Palauan, Sonsorolese-Tobian, and English are the official languages of Palau. Religion The indigenous Palauan religion of powerful ancestral and nature spirits was supplanted by Christianity, brought by missionaries. Slightly more than half the population is Roman Catholic; just over one-fourth is Protestant. There are smaller numbers of Seventh-day Adventists, Jehovah’s Witnesses, Mormons, and members of other faiths. Settlement patterns and demographic trends Historically, Palauans have tended to migrate overseas to a greater extent than have other Micronesians. There are a number of substantial Palauan communities on Guam, in Hawaii, and on the West Coast of the United States. Beginning in the late 20th century, immigration—fueled by foreigners seeking employment, especially those from the Philippines—grew significantly; by the early 21st century, foreigners accounted for more than one-fourth of the population. More … Score:

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Proclamation of the People's Republic of China

China, Chinese (Pinyin) Zhonghua or (Wade-Giles romanization) Chung-hua, also spelled (Pinyin) Zhongguo or (Wade-Giles romanization) Chung-kuo, officially People’s Republic of China or Chinese (Pinyin) Zhonghua Renmin Gongheguo or (Wade-Giles romanization) Chung-hua Jen-min Kung-ho-kuo, country of East Asia. It is the largest of all Asian countries and has the largest population of any country in the world. Occupying nearly the entire East Asian landmass, it covers approximately one-fourteenth of the land area of Earth. Among the major countries of the world, China is surpassed in area by only Russia and Canada, and it is almost as large as the whole of Europe. China has 33 administrative units directly under the central government; these consist of 22 provinces, 5 autonomous regions, 4 municipalities (Chongqing, Beijing, Shanghai, and Tianjin), and 2 special administrative regions (Hong Kong and Macau). The island province of Taiwan, which has been under separate administration since 1949, is discussed in the article Taiwan. Beijing (Peking), the capital of the People’s Republic, is also the cultural, economic, and communications centre of the country. Shanghai is the main industrial city; Hong Kong is the leading commercial centre and port. Within China’s boundaries exists a highly diverse and complex country. Its topography encompasses the highest and one of the lowest places on Earth, and its relief varies from nearly impenetrable mountainous terrain to vast coastal lowlands. Its climate ranges from extremely dry, desertlike conditions in the northwest to tropical monsoon in the southeast, and China has the greatest contrast in temperature between its northern and southern borders of any country in the world. The diversity of both China’s relief and its climate has resulted in one of the world’s widest arrays of ecological niches, and these niches have been filled by a vast number of plant and animal species. Indeed, practically all types of Northern Hemisphere plants, except those of the polar tundra, are found in China, and, despite the continuous inroads of humans over the millennia, China still is home to some of the world’s most exotic animals. Probably the single most identifiable characteristic of China to the people of the rest of the world is the size of its population. Some one-fifth of humanity is of Chinese nationality. The great majority of the population is Chinese (Han), and thus China is often characterized as an ethnically homogeneous country, but few countries have as wide a variety of indigenous peoples as does China. Even among the Han there are cultural and linguistic differences between regions; for example, the only point of linguistic commonality between two individuals from different parts of China may be the written Chinese language. Because China’s population is so enormous, the population density of the country is also often thought to be uniformly high, but vast areas of China are either uninhabited or sparsely populated. With more than 4,000 years of recorded history, China is one of the few existing countries that also flourished economically and culturally in the earliest stages of world civilization. Indeed, despite the political and social upheavals that frequently have ravaged the country, China is unique among nations in its longevity and resilience as a discrete politico-cultural unit. Much of China’s cultural development has been accomplished with relatively little outside influence, the introduction of Buddhism from India constituting a major exception. Even when the country was penetrated by such “barbarian” peoples as the Manchu, these groups soon became largely absorbed into the fabric of Han Chinese culture. This relative isolation from the outside world made possible over the centuries the flowering and refinement of the Chinese culture, but it also left China ill prepared to cope with that world when, from the mid-19th century, it was confronted by technologically superior foreign nations. There followed a century of decline and decrepitude, as China found itself relatively helpless in the face of a foreign onslaught. The trauma of this external challenge became the catalyst for a revolution that began in the early 20th century against the old regime and culminated in the establishment of a communist government in 1949. This event reshaped global political geography, and China has since come to rank among the most influential countries in the world. Central to China’s long-enduring identity as a unitary country is the province, or sheng (“secretariat”). The provinces are traceable in their current form to the Tang dynasty (618–907 ce). Over the centuries, provinces gained in importance as centres of political and economic authority and increasingly became the focus of regional identification and loyalty. Provincial power reached its peak in the first two decades of the 20th century, but, since the establishment of the People’s Republic, that power has been curtailed by a strong central leadership in Beijing. Nonetheless, while the Chinese state has remained unitary in form, the vast size and population of China’s provinces—which are comparable to large and midsize nations—dictate their continuing importance as a level of subnational administration. Land China stretches for about 3,250 miles (5,250 km) from east to west and 3,400 miles (5,500 km) from north to south. Its land frontier is about 12,400 miles (20,000 km) in length, and its coastline extends for some 8,700 miles (14,000 km). The country is bounded by Mongolia to the north; Russia and North Korea to the northeast; the Yellow Sea and the East China Sea to the east; the South China Sea to the southeast; Vietnam, Laos, Myanmar (Burma), India, Bhutan, and Nepal to the south; Pakistan to the southwest; and Afghanistan, Tajikistan, Kyrgyzstan, and Kazakhstan to the west. In addition to the 14 countries that border directly on it, China also faces South Korea and Japan, across the Yellow Sea, and the Philippines, which lie beyond the South China Sea. Relief of China Broadly speaking, the relief of China is high in the west and low in the east; consequently, the direction of flow of the major rivers is generally eastward. The surface may be divided into three steps, or levels. The first level is represented by the Plateau of Tibet, which is located in both the Tibet Autonomous Region and the province of Qinghai and which, with an average elevation of well over 13,000 feet (4,000 metres) above sea level, is the loftiest highland area in the world. The western part of this region, the Qiangtang, has an average height of 16,500 feet (5,000 metres) and is known as the “roof of the world.” The second step lies to the north of the Kunlun and Qilian mountains and (farther south) to the east of the Qionglai and Daliang ranges. There the mountains descend sharply to heights of between 6,000 and 3,000 feet (1,800 and 900 metres), after which basins intermingle with plateaus. This step includes the Mongolian Plateau, the Tarim Basin, the Loess Plateau (loess is a yellow-gray dust deposited by the wind), the Sichuan Basin, and the Yunnan-Guizhou (Yungui) Plateau. The third step extends from the east of the Dalou, Taihang, and Wu mountain ranges and from the eastern perimeter of the Yunnan-Guizhou Plateau to the China Sea. Almost all of this area is made up of hills and plains lying below 1,500 feet (450 metres). The most remarkable feature of China’s relief is the vast extent of its mountain chains; the mountains, indeed, have exerted a tremendous influence on the country’s political, economic, and cultural development. By rough estimate, about one-third of the total area of China consists of mountains. China has the world’s tallest mountain and the world’s highest and largest plateau, in addition to possessing extensive coastal plains. The five major landforms—mountain, plateau, hill, plain, and basin—are all well represented. China’s complex natural environment and rich natural resources are closely connected with the varied nature of its relief. The topography of China is marked by many splendours. Mount Everest (Qomolangma Feng), situated on the border between China and Nepal, is the highest peak in the world, at an elevation of 29,035 feet (8,850 metres; see Researcher’s Note: Height of Mount Everest). By contrast, the lowest part of the Turfan Depression in the Uygur Autonomous Region of Xinjiang—Lake Ayding—is 508 feet (155 metres) below sea level. The coast of China contrasts greatly between South and North. To the south of the bay of Hangzhou, the coast is rocky and indented with many harbours and offshore islands. To the north, except along the Shandong and Liaodong peninsulas, the coast is sandy and flat. China is prone to intense seismic activity throughout much of the country. The main source of this geologic instability is the result of the constant northward movement of the Indian tectonic plate beneath southern Asia, which has thrust up the towering mountains and high plateaus of the Chinese southwest. Throughout its history China has experienced hundreds of massive earthquakes that collectively have killed millions of people. Two in the 20th century alone—in eastern Gansu province (1920) and in the city of Tangshan, eastern Hebei province (1976)—caused some 250,000 deaths each, and a quake in east-central Sichuan province in 2008 killed tens of thousands and devastated a wide area. China’s physical relief has dictated its development in many respects. The civilization of Han Chinese originated in the southern part of the Loess Plateau, and from there it extended outward until it encountered the combined barriers of relief and climate. The long, protruding corridor, commonly known as the Gansu, or Hexi, Corridor, illustrates this fact. South of the corridor is the Plateau of Tibet, which was too high and too cold for the Chinese to gain a foothold. North of the corridor is the Gobi Desert, which also formed a barrier. Consequently, Chinese civilization was forced to spread along the corridor, where melting snow and ice in the Qilian Mountains provided water for oasis farming. The westward extremities of the corridor became the meeting place of the ancient East and West. Thus, for a long time the ancient political centre of China was located along the lower reaches of the Huang He (Yellow River). Because of topographical barriers, however, it was difficult for the central government to gain complete control over the entire country, except when an unusually strong dynasty was in power. In many instances the Sichuan Basin—an isolated region in southwestern China, about twice the size of Scotland, that is well protected by high mountains and is self-sufficient in agricultural products—became an independent kingdom. A comparable situation often arose in the Tarim Basin in the northwest. Linked to the rest of China only by the Gansu Corridor, this basin is even remoter than the Sichuan, and, when the central government was unable to exert its influence, oasis states were established; only the three strong dynasties—the Han (206 bce–220 ce), the Tang (618–907ce), and the Qing, or Manchu (1644–1911/12)—were capable of controlling the region. Apart from the three elevation zones already mentioned, it is possible—on the basis of geologic structure, climatic conditions, and differences in geomorphologic development—to divide China into three major topographic regions: the eastern, northwestern, and southwestern zones. The eastern zone is shaped by the rivers, which have eroded landforms in some parts and have deposited alluvial plains in others; its climate is monsoonal (characterized by seasonal rain-bearing winds). The northwestern region is arid and eroded by the wind; it forms an inland drainage basin. The southwest is a cold, lofty, and mountainous region containing intermontane plateaus and inland lakes. The three basic regions may be further subdivided into second-order geographic divisions. The eastern region contains 10 of these, the southwest contains two, and the northwest contains three. Below is a brief description of each division. more … Score:

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