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Meydan Dağ
Mount Meydan (), is an extinct Volcano located in the provincial borders of Van and Ağrı. It is located 7 kilometers northwest of Erciş city. Inside the mountain is a crater and caldera. Overview Meydan Mountain is located at the zero point of the border of Patnos district of Ağrı and Erciş district of Van. Its highest point is 2778 meters with Gürgür Mountain. The base of the caldera is 2320 m. With the collection of surrounding waters in the caldera, the caldera lake was formed. The waters coming out of this lake form the Meydan Stream. Gürgürbaba consists of a relatively soft sloping and symmetrical round dome. See also * List of volcanoes in Turkey * Mount Nemrut * Akdoğan Mountains Akdoğan Mountains (); (); is a mountain range located at the zero point of the Muş and Erzurum border. It extends from the east of Akdoğan lake to Karaçoban district by crossing the border where Varto, Bulanık and Hınıs districts inter ... References Stratovolcanoes of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Turkey
Turkey, officially the Republic of Türkiye, is a country mainly located in Anatolia in West Asia, with a relatively small part called East Thrace in Southeast Europe. It borders the Black Sea to the north; Georgia (country), Georgia, Armenia, Azerbaijan, and Iran to the east; Iraq, Syria, and the Mediterranean Sea to the south; and the Aegean Sea, Greece, and Bulgaria to the west. Turkey is home to over 85 million people; most are ethnic Turkish people, Turks, while ethnic Kurds in Turkey, Kurds are the Minorities in Turkey, largest ethnic minority. Officially Secularism in Turkey, a secular state, Turkey has Islam in Turkey, a Muslim-majority population. Ankara is Turkey's capital and second-largest city. Istanbul is its largest city and economic center. Other major cities include İzmir, Bursa, and Antalya. First inhabited by modern humans during the Late Paleolithic, present-day Turkey was home to List of ancient peoples of Anatolia, various ancient peoples. The Hattians ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paris 1 Panthéon-Sorbonne University
Paris 1 Panthéon-Sorbonne University (), also known as Paris 1 (or Paris I) and Panthéon-Sorbonne University (or, together with Sorbonne University and Sorbonne Nouvelle University, simply as the Sorbonne), is a Public university, public research university in Paris, France. It was created in 1971 from two faculties of the historic University of Paris – colloquially referred to as the Sorbonne – after the May 68, May 1968 protests, which resulted in the division of one of the world's oldest universities. Most of the economics professors (35 out of 41) of the Faculty of Law and Economics of Paris decided to found the multidisciplinary Paris 1 University with professors of the faculty of humanities of Paris and a few professors of law. Panthéon-Sorbonne has three main areas of specialization: Economics and Management, Human Sciences, and Legal and Political Sciences. It comprises several subjects such as: Economics, Law, Philosophy, Sociology, History, Geography, Film, Cin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanic Crater Lakes
A volcano is commonly defined as a vent or fissure in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and because most of Earth's plate boundaries are underwater, most volcanoes are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes resulting from divergent tectonic activity are usually non-explosive whereas those resulting from convergent tectonic activity cause violent eruptions."Mid-ocean ridge tectonics, volcanism and geomorphology." Geology 26, no. 455 (2001): 458. https://macdonald.faculty.geol.ucsb.edu/papers/Macdonald%20Mid-Ocean%20Ridge%20Tectonics.pdf Volcanoes can also form where there is stretching an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Calderas Of Turkey
A caldera ( ) is a large cauldron-like hollow that forms shortly after the emptying of a magma chamber in a volcanic eruption. An eruption that ejects large volumes of magma over a short period of time can cause significant detriment to the structural integrity of such a chamber, greatly diminishing its capacity to support its own roof and any substrate or rock resting above. The ground surface then collapses into the emptied or partially emptied magma chamber, leaving a large depression at the surface (from one to dozens of kilometers in diameter). Although sometimes described as a crater, the feature is actually a type of sinkhole, as it is formed through subsidence and collapse rather than an explosion or impact. Compared to the thousands of volcanic eruptions that occur over the course of a century, the formation of a caldera is a rare event, occurring only a few times within a given window of 100 years. Only eight caldera-forming collapses are known to have occurred between ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stratovolcanoes Of Turkey
A stratovolcano, also known as a composite volcano, is a typically conical volcano built up by many alternating layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and explosive eruptions. Some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and solidifies before spreading far, due to high viscosity. The magma forming this lava is often felsic, having high to intermediate levels of silica (as in rhyolite, dacite, or andesite), with lesser amounts of less viscous mafic magma. Extensive felsic lava flows are uncommon, but can travel as far as 8 km (5 mi). The term ''composite volcano'' is used because strata are usually mixed and uneven instead of neat layers. They are among the most common types of volcanoes; more than 700 stratovolcanoes have erupted lava during the Holocene Epoch (the last 11,700 years), and many older, now ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Akdoğan Mountains
Akdoğan Mountains (); (); is a mountain range located at the zero point of the Muş and Erzurum border. It extends from the east of Akdoğan lake to Karaçoban district by crossing the border where Varto, Bulanık and Hınıs districts intersect. Geology and geomorphology Akdoğan mountains appear as a mountain mass between the Hınıs Plain and the Murat river. It includes Akdoğan Lake, one of Turkey's highest and well-preserved lakes. It has rich water resources and some parts of the mountain consist of calcareous layers. Akdoğan Mountains are one of the important wetlands for birds and there are more than 100 small and shallow lakes on it. Most of the lakes are located around the Hınıs villages, located north of the 2879 meter peak. Akdoğan Mountains are one of the highest mountains in Muş province and have the most organized forests. The width of the Akdoğan mountains is 10 km and the length is 30 km. As a result of the volcanic eruptions in the Akdoğan M ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nemrut (volcano)
Nemrut (, ''Sarakn'', "Mountain spring", , ) is a dormant volcano in Tatvan district, Bitlis province, Eastern Turkey, close to Lake Van. The volcano is named after King Nimrod who is said to have ruled this area in about 2100 BC. There is Lake Nemrut in the crater of the mountain. The most powerful eruptions of Nemrut occurred in the Pleistocene. Many small eruptions occurred during the Holocene, the last in 1650. The top of the volcano is a large caldera hosting three crater lakes. Overview Nemrut is a polygenetic stratovolcano located in the collision zone of the Arabian and Eurasian tectonic plates, which determines the seismic and volcanic activity in the region. The collision of these plates began in the Middle Eocene and closed the stretch of water, which in the Mesozoic formed the Tethys Ocean. Nemrut, along with three other volcanoes of eastern Turkey: Ararat, Tendürek and Süphan, is located in the area of a complex fault, which runs along the boundary of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Volcanoes In Turkey ...
This is a list of dormant and extinct volcanoes in Turkey. See also * Geology of Turkey * Geothermal power in Turkey References {{Global Volcanism Program * Volcanoes Turkey Turkey, officially the Republic of Türkiye, is a country mainly located in Anatolia in West Asia, with a relatively small part called East Thrace in Southeast Europe. It borders the Black Sea to the north; Georgia (country), Georgia, Armen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Patnos District
Patnos District is a district of Ağrı Province of Turkey. Its seat is the town Patnos.İlçe Belediyesi Turkey Civil Administration Departments Inventory. Retrieved 12 January 2023. Its area is 1,394 km2, and its population is 118,481 (2021). Composition There are two in Patnos District: * Dedeli * There are 92 |
Armenian Highlands
The Armenian highlands (; also known as the Armenian upland, Armenian plateau, or Armenian tableland)Robert Hewsen, Hewsen, Robert H. "The Geography of Armenia" in ''The Armenian People From Ancient to Modern Times Volume I: The Dynastic Periods: From Antiquity to the Fourteenth Century''. Richard G. Hovannisian (ed.) New York: St. Martin's Press, 1997, pp. 1–17 comprise the most central and the highest of the three plateaus that together form the northern sector of West Asia. Clockwise starting from the west, the Armenian highlands are bounded by the Anatolia, Anatolian plateau, the Caucasus, the Kur-Araz Lowland, Kura-Aras lowlands, the Iranian Plateau, and Mesopotamia. The highlands are divided into western and eastern regions, defined by the Ararat Plain, Ararat Valley where Mount Ararat is located. Western Armenia is nowadays referred to as Eastern Anatolia. On the other hand, Eastern Armenia is part of Lesser Caucasus or Caucasus Minor, which was historically known by some ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Erciş
Erciş (; ; , historically , ''Arčeš'') is a municipality and district of Van Province, Turkey. Its area is 2,133 km2, and its population is 171,000 (2022). It is located at the northern end of Lake Van. History of Artchesh During Classical Antiquity, the town was known as Arsissa, and Archesh (Arčeš) in Armenian and Arjish in Arabic. The Byzantines knew it as Arzes (Ἂρζες or Ἀρζές) and the 10th-century emperor Constantine VII Porphyrogennetos wrote in his ''De administrando imperio'' (Chapter XLIV) that it was under the rule of the Kaysite emirate of Manzikert. This small district served as the capital city of a number of ruling states. It was the main center of the province of Turuberan as part of the ancient Kingdom of Armenia. The city changed hands on several occasions between the Arabs and the Byzantines, in the early Middle Ages. From the mid 1020s onwards Archesh was governed by the Byzantines. In 1054, it was captured and sacked by the Selj ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
