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Guinea News - TransAfrica

It could also derive from the Berber Akal n-Iguinawen, “land of the blacks”. Surprising country for the variety of landscapes. From its mountains three rivers ...

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2024/10/04

Timeless Tuvalu – Welcome to the official tourism site for ...

Welcome To Timeless Tuvalu Our Paradise Is Waiting · Funafuti Marine Conservation · Diving and Snorkeling · Cultural and Traditional Dance · Save Tuvalu ·

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2024/10/03

Palau Pledge · ‎Visiting Palau · ‎Find Stay In Palau · ‎Palau Visitors Authority

Nestled in the western Pacific Ocean, southwest of Guam, is a cluster of islands that make up this Pristine Paradise. · Palau is a world-renowned premier diving ...

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2024/10/03

Lesotho: The country Inside South Africa

Lesotho is a country inside of a country. It is an enclave and the largest in the world at that. How did the country of Lesotho come to be? Why is Maseru it's capital and why is it not a part of South Africa?

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2024/10/03

National Day of the Republic of Iraq

Iraq, country of southwestern Asia. During ancient times, lands that now constitute Iraq were known as Mesopotamia (“Land Between the Rivers”), a region whose extensive alluvial plains gave rise to some of the world’s earliest civilizations, including those of Sumer, Akkad, Babylon, and Assyria. This wealthy region, comprising much of what is called the Fertile Crescent, later became a valuable part of larger imperial polities, including sundry Persian, Greek, and Roman dynasties, and after the 7th century it became a central and integral part of the Islamic world. Iraq’s capital, Baghdad, became the capital of the Abbasid Caliphate in the 8th century. The modern nation-state of Iraq was created following World War I (1914–18) from the Ottoman provinces of Baghdad, Basra, and Mosul and derives its name from the Arabic term used in the premodern period to describe a region that roughly corresponded to Mesopotamia (ʿIrāq ʿArabī, “Arabian Iraq”) and modern northwestern Iran (ʿIrāq ʿAjamī, “foreign [i.e., Persian] Iraq”). Iraq gained formal independence in 1932 but remained subject to British imperial influence during the next quarter century of turbulent monarchical rule. Political instability on an even greater scale followed the overthrow of the monarchy in 1958, but the installation of an Arab nationalist and socialist regime—the Baʿath Party—in a bloodless coup 10 years later brought new stability. With proven oil reserves second in the world only to those of Saudi Arabia, the regime was able to finance ambitious projects and development plans throughout the 1970s and to build one of the largest and best-equipped armed forces in the Arab world. The party’s leadership, however, was quickly assumed by Saddam Hussein, a flamboyant and ruthless autocrat who led the country into disastrous military adventures—the Iran-Iraq War (1980–88) and the Persian Gulf War (1990–91). These conflicts left the country isolated from the international community and financially and socially drained, but—through unprecedented coercion directed at major sections of the population, particularly the country’s disfranchised Kurdish minority and the Shiʿi majority—Saddam himself was able to maintain a firm hold on power into the 21st century. He and his regime were toppled in 2003 during the Iraq War. Land Iraq is one of the easternmost countries of the Arab world, located at about the same latitude as the southern United States. It is bordered to the north by Turkey, to the east by Iran, to the west by Syria and Jordan, and to the south by Saudi Arabia and Kuwait. Iraq has 36 miles (58 km) of coastline along the northern end of the Persian Gulf, giving it a tiny sliver of territorial sea. Followed by Jordan, it is thus the Middle Eastern state with the least access to the sea and offshore sovereignty. Relief Iraq’s topography can be divided into four physiographic regions: the alluvial plains of the central and southeastern parts of the country; Al-Jazīrah (Arabic: “the Island”), an upland region in the north between the Tigris and Euphrates rivers; deserts in the west and south; and the highlands in the northeast. Each of these regions extends into neighbouring countries, although the alluvial plains lie largely within Iraq. Alluvial plains The plains of lower Mesopotamia extend southward some 375 miles (600 km) from Balad on the Tigris and Al-Ramādī on the Euphrates to the Persian Gulf. They cover more than 51,000 square miles (132,000 square km), almost one-third of the country’s area, and are characterized by low elevation, below 300 feet (100 metres), and poor natural drainage. Large areas are subject to widespread seasonal flooding, and there are extensive marshlands, some of which dry up in the summer to become salty wastelands. Near Al-Qurnah, where the Tigris and Euphrates converge to form the Shaṭṭ al-ʿArab, there are still some inhabited marshes. The alluvial plains contain extensive lakes. The swampy Lake Al-Ḥammār (Hawr al-Ḥammār) extends 70 miles (110 km) from Basra (Al-Baṣrah) to Sūq al-Shuyūkh; its width varies from 8 to 15 miles (13 to 25 km). Al-Jazīrah North of the alluvial plains, between the Tigris and the Euphrates rivers, is the arid Al-Jazīrah plateau. Its most prominent hill range is the Sinjār Mountains, whose highest peak reaches an elevation of 4,448 feet (1,356 metres). The main watercourse is the Wadi Al-Tharthār, which runs southward for 130 miles (210 km) from the Sinjār Mountains to the Tharthār (Salt) Depression. Milḥat Ashqar is the largest of several salt flats (or sabkhahs) in the region. Deserts Western and southern Iraq is a vast desert region covering some 64,900 square miles (168,000 square km), almost two-fifths of the country. The western desert, an extension of the Syrian Desert, rises to elevations above 1,600 feet (490 metres). The southern desert is known as Al-Ḥajarah in the western part and as Al-Dibdibah in the east. Al-Ḥajarah has a complex topography of rocky desert, wadis, ridges, and depressions. Al-Dibdibah is a more sandy region with a covering of scrub vegetation. Elevation in the southern desert averages between 300 and 1,200 feet (100 to 400 metres). A height of 3,119 feet (951 metres) is reached at Mount ʿUnayzah (ʿUnāzah) at the intersection of the borders of Jordan, Iraq, and Saudi Arabia. The deep Wadi Al-Bāṭin runs 45 miles (75 km) in a northeast-southwest direction through Al-Dibdibah. It has been recognized since 1913 as the boundary between western Kuwait and Iraq. The northeast of Iraq The mountains, hills, and plains of northeastern Iraq occupy some 35,500 square miles (92,000 square km), about one-fifth of the country. Of this area only about one-fourth is mountainous; the remainder is a complex transition zone between mountain and lowland. The ancient kingdom of Assyria was located in this area. North and northeast of the Assyrian plains and foothills is Kurdistan, a mountainous region that extends into Turkey and Iran. The relief of northeastern Iraq rises from the Tigris toward the Turkish and Iranian borders in a series of rolling plateaus, river basins, and hills until the high mountain ridges of Iraqi Kurdistan, associated with the Taurus and Zagros mountains, are reached. These mountains are aligned northwest to southeast and are separated by river basins where human settlement is possible. The mountain summits have an average elevation of about 8,000 feet (2,400 metres), rising to 10,000–11,000 feet (3,000–3,300 metres) in places. There, along the Iran-Iraq border, is the country’s highest point, Ghundah Zhur, which reaches 11,834 feet (3,607 metres). The region is heavily dissected by numerous tributaries of the Tigris, notably the Great and Little Zab rivers and the Diyālā and ʿUẓaym (Adhaim) rivers. These streams weave tortuously south and southwest, cutting through ridges in a number of gorges, notably the Rū Kuchūk gorge, northeast of Barzān, and the Bēkma gorge, west of Rawāndūz town. The highest mountain ridges contain the only forestland in Iraq. More … Score: https://www.britannica.com/place/Iraq  

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2024/10/03

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: https://www.britannica.com/place/Germany

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2024/10/03

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