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2026/10/31

GoTürkiye: Official Travel Guide of Türkiye

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2026/10/31

Republic of Turkey Day of the Republic

Turkey, country that occupies a unique geographic position, lying partly in Asia and partly in Europe. Throughout its history it has acted as both a barrier and a bridge between the two continents. Turkey is situated at the crossroads of the Balkans, Caucasus, Middle East, and eastern Mediterranean. It is among the larger countries of the region in terms of territory and population, and its land area is greater than that of any European state. Nearly all of the country is in Asia, comprising the oblong peninsula of Asia Minor—also known as Anatolia (Anadolu)—and, in the east, part of a mountainous region sometimes known as the Armenian Highland. The remainder—Turkish Thrace (Trakya)—lies in the extreme southeastern part of Europe, a tiny remnant of an empire that once extended over much of the Balkans. The country has a north-south extent that ranges from about 300 to 400 miles (480 to 640 km), and it stretches about 1,000 miles from west to east. Turkey is bounded on the north by the Black Sea, on the northeast by Georgia and Armenia, on the east by Azerbaijan and Iran, on the southeast by Iraq and Syria, on the southwest and west by the Mediterranean Sea and the Aegean Sea, and on the northwest by Greece and Bulgaria. The capital is Ankara, and its largest city and seaport is Istanbul. Of a total boundary length of some 4,000 miles (6,440 km), about three-fourths is maritime, including coastlines along the Black Sea, the Aegean, and the Mediterranean, as well as the narrows that link the Black and Aegean seas. These narrows—which include the Bosporus, the Sea of Marmara, and the Dardanelles—are known collectively as the Turkish straits; Turkey’s control of the straits, the only outlet from the Black Sea, has been a major factor in its relations with other states. Most of the islands along the Aegean coast are Greek; only the islands of Gökçeada and Bozcaada remain in Turkish hands. The maritime boundary with Greece has been a source of dispute between the two countries on numerous occasions since World War II. A long succession of political entities existed in Asia Minor over the centuries. Turkmen tribes invaded Anatolia in the 11th century ce, founding the Seljuq empire; during the 14th century the Ottoman Empire began a long expansion, reaching its peak during the 17th century. The modern Turkish republic, founded in 1923 after the collapse of the Ottoman Empire, is a nationalist, secular, parliamentary democracy. After a period of one-party rule under its founder, Mustafa Kemal (Atatürk), and his successor, Turkish governments since the 1950s have been produced by multiparty elections based on universal adult suffrage. Land - Relief Turkey is a predominantly mountainous country, and true lowland is confined to the coastal fringes. About one-fourth of the surface has an elevation above 4,000 feet (1,200 metres), and less than two-fifths lies below 1,500 feet (460 metres). Mountain crests exceed 7,500 feet (2,300 metres) in many places, particularly in the east, where Turkey’s highest mountain, Mount Ararat (Ağrı), reaches 16,945 feet (5,165 metres) close to the borders with Armenia and Iran. In the southeast the Uludoruk Peak reaches 15,563 feet (4,744 metres); though further west, the Demirkazık Peak (12,320 feet [3,755 metres]) and Mount Aydos (11,414 feet [3,479 metres]) are also significant peaks. Steep slopes are common throughout the country, and flat or gently sloping land makes up barely one-sixth of the total area. These relief features affect other aspects of the physical environment, producing climates often much harsher than might be expected for a country of Turkey’s latitude and reducing the availability and productivity of agricultural land. Structurally, the country lies within the geologically young folded-mountain zone of Eurasia, which in Turkey trends predominantly east to west. The geology of Turkey is complex, with sedimentary rocks ranging from Paleozoic to Quaternary, numerous intrusions, and extensive areas of volcanic material. Four main regions can be identified: the northern folded zone, the southern folded zone, the central massif, and the Arabian platform. The northern folded zone The northern folded zone comprises a series of mountain ridges, increasing in elevation toward the east, that occupy a belt about 90 to 125 miles (145 to 200 km) wide immediately south of the Black Sea. The system as a whole is referred to as the Pontic Mountains (Doğukaradeniz Dağları). In the west the system has been fractured by the faulting that produced the Turkish straits; in Thrace the Ergene lowlands are among the largest in the country, and the main mountain range—the Yıldız (Istranca)—reaches only 3,379 feet (1,030 metres). Lowlands also occur to the south of the Sea of Marmara and along the lower Sakarya River east of the Bosporus. High ridges trending east-west rise abruptly from the Black Sea coast, and the coastal plain is thus narrow, opening out only in the deltas of the Kızıl and Yeşil rivers. These rivers break through the mountain barrier in a zone of weakness where summits are below 2,000 feet (600 metres), dividing the Pontic Mountains into western and eastern sections. In the western section, between the Sakarya and Kızıl rivers, there are four main ridges: the Küre, Bolu, Ilgaz, and Köroğlu mountains. East of the Yeşil the system is higher, narrower, and steeper. Less than 50 miles from the coast, peaks rise to more than 10,000 feet (3,000 metres), with a maximum elevation of 12,917 feet (3,937 metres) in the Kaçkar range. Separated by the narrow trough of the Kelkit and Çoruh river valleys stands a second ridge that rises above 8,000 feet (2,400 metres). The southern folded zone The southern folded zone occupies the southern third of the country, from the Aegean to the Gulf of Iskenderun, from which it extends to the northeast and east around the northern side of the Arabian platform. Over most of its length, the Mediterranean coastal plain is narrow, but there are two major lowland embayments. The Antalya Plain extends inland some 20 miles (30 km) from the Gulf of Antalya; the Adana Plain, measuring roughly 90 by 60 miles (145 by 100 km), comprises the combined deltas of the Seyhan and Ceyhan rivers. The mountain system falls into two main parts. West of Antalya a complex series of ridges with a north-south trend reaches 6,500 to 8,200 feet (2,000 to 2,500 metres), but the most prominent feature is the massive Taurus (Toros) mountain system, running parallel to the Mediterranean coast and extending along the southern border. There crest lines are often above 8,000 feet (2,400 metres), and several peaks exceed 11,000 feet (3,400 metres). In the eastern third of the country, the northern and southern fold systems converge to produce an extensive area of predominantly mountainous terrain, with pockets of relatively level land confined to valleys and enclosed basins, as are found around Malatya, Elazığ, and Muş. The central massif The central massif is located in the western half of the country, between the Pontic and Taurus systems. This elevated zone is often referred to as the Anatolian plateau, although its relief is much more varied than this term suggests. At least four subdivisions of the central massif can be identified. Inland from the Aegean as far as a line from Bursa to Denizli, a series of faulted blocks gives a north-south alternation of steep-sided plateaus rising 5,000–6,500 feet (1,500–2,000 metres) and low-lying valley floors. Alluvial plains along the larger rivers, such as the Gediz, Küçükmenderes, and Büyükmenderes, are among the largest in Turkey and are of special agricultural value. East of this section, roughly to a line from Eskişehir to Burdur, is a complex upland zone. The general surface level rises to the east from 1,500 to 3,000 feet (460 to 900 metres); set into the upland are several downfaulted basins, and above it short mountain ranges rise to 6,500 feet. The most distinctive part of the central massif is the area bounded on the south by the Taurus Mountains and on the northeast by a line from Ankara through Lake Tuz to Niğde. There the term plateau is most applicable, with large expanses of flat or gently sloping land at elevations of about 3,000 feet separated by low upswellings in the surface. Measuring some 150 by 200 miles (240 by 320 km), these are by far the most extensive plains in Turkey; however, their agricultural value is reduced by the effects of altitude and location on their climate. The remainder of the central massif, a roughly triangular area with its eastern apex near Sivas, forms a mountainous zone that bounds the plains on their eastern side. Much of this section rises above 5,000 feet (1,500 metres), and there are numerous peaks with elevations of about 6,500 feet. A noteworthy feature is the extensive area of geologically recent volcanic activity in Niğde, Nevşehir, and Kayseri provinces, including the volcanic peaks of Erciyes (12,848 feet [3,916 metres]) and Hasan (10,686 feet [3,257 metres]). More … Score: https://www.britannica.com/place/Turkey  

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2026/10/29

Discover SVG: Explore St. Vincent and the Grenadines

One Destination, 32 Islands and Cays, countless possibilities. From St. Vincent's lush tropical rainforest full of eco-adventures, to the idyllic beaches, coral ...

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2026/10/29

Turkey Promotion- Go Turkey

Türkiye tanıtım videosu, T.C. Kültür ve Turizm Bakanlığının hazırladığı videodur #turkey #biciktv

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2026/10/28

Czech Republic Independence Proclamation

Czech Republic, also called Czechia, country located in central Europe. It comprises the historical provinces of Bohemia and Moravia along with the southern tip of Silesia, collectively often called the Czech Lands. In 2016 the country adopted the name “Czechia” as a shortened, informal name for the Czech Republic. Despite its landlocked location, there were brief periods in the Middle Ages during which Bohemia had access to the Baltic and Adriatic seacoasts—which no doubt was on William Shakespeare’s mind when he set much of his play The Winter’s Tale there. A region of rolling hills and mountains, Bohemia is dominated by the national capital, Prague. Set on the Vltava River, this picturesque city of bridges and spires is the unique work of generations of artists brought in by the rulers of Bohemia. Perhaps only the French are as focused on their capital, Paris, as the Czechs are on theirs; of the two, Prague has a more magical quality for many. Called “the handsomest city of Europe” since the 18th century, it has intoxicated writers, poets, and musicians alike. While Prague was the birthplace of the writer Franz Kafka and the poet Rainer Maria Rilke, Brno, Moravia’s largest city, was the site of Gregor Mendel’s groundbreaking genetic experiments in the 19th century and the birthplace of contemporary novelist Milan Kundera. Moravians are as proud of their vineyards and wine as Bohemians are of their breweries and the Pilsner beer that originated in the town of Plzeň (Pilsen), which is also noted as the site of the &Scaron;koda Works—a heavy industrial complex that originated with the Habsburg monarchy. Moravia was equally endowed with skilled labour, which helped make Brno into one of the leading industrial towns in textiles and engineering during the 19th century and Ostrava, in the north, into a major coal-mining region, thanks to the vast fossil fuel deposits stretching over from Silesia. History is always close at hand in the Czech Republic, where stunning castles such as Karl&scaron;tejn (former keep of the royal crown of St. Wenceslas) and manor houses dot the landscape and medieval town centres abound. During its 1,000-year history, the country has changed shape and reshuffled its population. As the kingdom of Bohemia, it reached its zenith of wealth and power during the 13th and 14th centuries. Through a multitude of cultural, economic, ecclesiastical, and dynastic links, Bohemian kings became directly involved in the affairs of the German rulers of the Holy Roman Empire and opened the country to German colonization, which brought prosperity through silver mining and rapid urbanization. Prague, with the oldest university north of the Alps (Charles University, 1348), functioned as a royal and imperial capital. However, German colonization, which soon accounted for one-third of the total population and disadvantaged the majority Czechs, brought the seeds of discontent, resulting in an ugly, insolvable conflict in the 20th century. In the early 15th century Bohemia witnessed the Hussite revolution, a pre-Reformation movement named for Jan Hus, a follower of the English theologian and reformer John Wycliffe. Religious antagonism prevailed over ethnic tensions when Czechs and Germans jointly led the Protestant uprising that started the Thirty Years’ War (1618–48) against the Catholic Habsburgs, the Austro-German dynasty that ruled Bohemia from 1526 to 1918. After the Habsburg victory, the German language replaced Czech for almost two centuries—until the Czechs experienced an extraordinary linguistic and cultural revival that coincided with the revolutions of 1848 and the spread of industrialization. In historian Franti&scaron;ek Palacký and composers such as Bedřich Smetana and Antonín Dvořák, Czech nationalism found its ideal spokesmen. The collapse of the Austro-Hungarian Empire at the end of World War I brought the Czechs and Slovaks together for the first time as “Czechoslovaks.” The Czechs became the ruling ethnic group in Czechoslovakia, a new state in which Germans and Hungarians lived as unwilling citizens, bound to become disloyal minorities bent on undermining the democratic constitution engendered by the country’s founders, Tomá&scaron; G. Masaryk and Edvard Bene&scaron;. Many among this German population turned into Nazi sympathizers with the ascent to power of Adolf Hitler in Germany, whose design on the German-speaking border region of Czechoslovakia was appeased by England and France in the Munich Agreement of September 1938. Emasculated, Czechoslovakia succumbed to direct German invasion six months later. Bohemia and Moravia became a protectorate of the “Greater German Empire,” while Slovakia—whose Hungarian districts were ceded to Hungary—was induced by Hitler to proclaim its independence. After six years of brutal Nazi occupation (with its legacy of the Holocaust and the postwar mass expulsion of some three million Bohemian and Slovak [Carpathian] Germans), Czechoslovakia was reconstituted, this time without Ruthenia (Transcarpathian Ukraine), which was annexed by the Soviet Union. A communist coup in February 1948 sealed Czechoslovakia’s fate as a member of the Soviet bloc for the entire Cold War—though briefly, in the Prague Spring of 1968, a reform movement took over, only to be crushed by Soviet military invasion in August of that year. Still, that experience of freedom produced an underground dissident movement, later called Charter 77, whose leader, playwright Václav Havel, was propelled from prison to the royal castle, becoming the first president of postcommunist Czechoslovakia with the fall of the Berlin Wall in 1989. The last modification of the modern Czech nation-state was inaugurated on January 1, 1993, when the union with Slovakia was dissolved. As the Czech Republic, the new country joined the North Atlantic Treaty Organization (NATO) in 1999 and the European Union (EU) in 2004. Land of the Czech RepublicRelief The country is bordered by Poland to the north and northeast, Slovakia to the east, Austria to the south, and Germany to the west and northwest. The Bohemian Massif occupies the major portion of the Czech Republic. It consists of a large, roughly ovoid elevated basin (the Bohemian Plateau) encircled by mountains divided into six major groups. In the southwest are the &Scaron;umava Mountains, which include the Bohemian Forest (Böhmerwald). In the west are the Berounka River highlands. In the northwest, the Ore Mountains (Czech: Kru&scaron;né hory; German: Erzgebirge) form the frontier with Germany. The point at which the Elbe (Labe) River breaches this range is the lowest in the country, with an elevation of 384 feet (117 metres). The so-called Sudeten system of mountains (a name never applied in the Czech language) in the northeast forms most of the border with Poland west of the city of Ostrava. The highest point in the Czech Republic, Mount Sněžka, with an elevation of 5,256 feet (1,602 metres), is found in the major segment of this system, the Giant Mountains (Czech: Krkono&scaron;e; German: Riesengebirge). Farther to the east is the Oder (Odra) River lowland, a small fringe along the Polish border. Finally, southeast of the Bohemian Plateau are the Bohemian-Moravian Highlands, which include the spectacular Moravian Karst. In the east the Outer Carpathian Depressions, known to geographers as the Moravian-Silesian Beskids, include the valleys of the upper Oder and Morava rivers and the headstreams of the Dyje. Along the Czech-Slovak border rise the Little Carpathian (Bílé Karpaty) and Javorníky ranges, the westernmost of the Western Carpathian Mountains that dominate Slovakia. Drainage and soils The Czech Republic lies in the headwater area of the central European watershed. The Elbe River rises near the Czech-Polish border and sweeps southwestward across Bohemia, receiving the Jizera, Vltava, and Ohře rivers before flowing northward into Germany. The Vltava is navigable from Prague to Mělník, where it empties into the Elbe. From that point onward river traffic can travel all the way to Hamburg. The Morava River, flowing south toward the Danube (Dunaj) River, drains most of Moravia in the east. The Oder River rises in the northeastern Czech Republic and flows northward into Poland. There also are many smaller rivers of little economic importance. Larger rivers such as the Vltava are sources of hydroelectric power. The country is rich in mineral springs, and groundwater reserves are extensively used. The soil profile of the Czech Republic consists of some rich, black chernozems and good-quality brown soils in the drier and lower areas. Podzols are found in the wet districts, and stony mountain soils are typical at high elevations. Alluvial soils occur in the river basins, and heavy clay soils are found in the eastern ridges. Climate The Czech climate is mixed. Continental influences are marked by large fluctuations in both temperature and precipitation, while moderating oceanic influences diminish from west to east. In general, temperatures decrease with increasing elevation but are relatively uniform across the lower portions of the country. The mean annual temperature at Cheb in the extreme west is 45 °F (7 °C) and rises to only 48 °F (9 °C) at Brno in southern Moravia. High temperatures can exceed 90 °F (32 °C) in Prague during July, and low temperatures may drop as low as 0 °F (−17 °C) in Cheb during February. The growing season is about 200 days in the south but less than half that in the mountains. Annual precipitation ranges from 18 inches (450 mm) in the central Bohemian basins to more than 60 inches (1500 mm) on windward slopes of the Krkono&scaron;e Mountains of the north. Maximum precipitation falls during July, while the minimum occurs in February. There are no recognizable climatic zones but rather a succession of small and varied districts; climate thus follows the topography in contributing to the diversity of the natural environment. More … Score: https://www.britannica.com/place/Czech-Republic  

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2026/10/28

Biuletyn dyplomatyczny

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