Karapınar Field
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Karapınar Field
Karapınar Field is a volcanic field in central Anatolia, Asian Turkey. Geography The volcanic area is located near the city of Karapınar, in the Karapınar District of Konya Province. Features The basaltic Karapınar Volcanic Field consists of five cinder cones, two lava fields, and several explosion craters and maars. Meke Dağı, at in elevation, is one of the largest cinder cones in the Central Anatolia Region. Meke Dağı is surrounded by Meke Gölü, a crater lake. See also * Geology of Turkey * List of volcanoes in Turkey ** Karaca Dağ near Diyarbakır Diyarbakır (; ; ; ) is the largest Kurdish-majority city in Turkey. It is the administrative center of Diyarbakır Province. Situated around a high plateau by the banks of the Tigris river on which stands the historic Diyarbakır Fortress, ... References * Volcanoes of Turkey Volcanic fields Geology of Turkey Maars of Turkey Cinder cones Volcanic crater lakes Landforms of Konya Province ...
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Cinder Cone
A cinder cone (or scoria cone) is a steep conical hill of loose pyroclastic fragments, such as volcanic clinkers, volcanic ash, or scoria that has been built around a volcanic vent. The pyroclastic fragments are formed by explosive eruptions or lava fountains from a single, typically cylindrical, vent. As the gas-charged lava is blown violently into the air, it breaks into small fragments that solidify and fall as either cinders, clinkers, or scoria around the vent to form a cone that often is symmetrical; with slopes between 30 and 40°; and a nearly circular ground plan. Most cinder cones have a bowl-shaped crater at the summit. Mechanics of eruption Cinder cones range in size from tens to hundreds of meters tall and often have a bowl-shaped crater at the summit. They are composed of loose pyroclastic material (cinder or scoria), which distinguishes them from ''spatter cones'', which are composed of agglomerated volcanic bombs. The pyroclastic material making up a cinder ...
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Central Anatolia Region, Turkey
The Central Anatolia Region ( tr, İç Anadolu Bölgesi) is a geographical region of Turkey. The largest city in the region is Ankara. Other big cities are Konya, Kayseri, Eskişehir, Sivas, and Aksaray. Located in Central Turkey, it is bordered by the Aegean Region to the west, the Black Sea region to the north, the Eastern Anatolia Region to the east, and the Mediterranean Region to the south. It also shares a very slight border with the Marmara Region in Bilecik Province. Cities Cities located in Central Anatolia: Subdivisions * Konya Section ( tr, Konya Bölümü) ** Obruk Plateau ( tr, Obruk Platosu) ** Konya - Ereğli Vicinity ( tr, Konya - Ereğli Çevresi) * Upper Sakarya Section ( tr, Yukarı Sakarya Bölümü) ** Ankara Area ( tr, Ankara Yöresi) ** Porsuk Gully ( tr, Porsuk Oluğu) ** Sündiken Mountain Chain Area ( tr, Sündiken Dağları Yöresi) ** Upper Sakarya Gully ( tr, Yukarı Sakarya Yöresi) * Middle Kızılırmak Section ( tr, Orta Kızılı ...
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Landforms Of Konya Province
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fou ...
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Volcanic Crater Lakes
A volcano is a rupture 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 most 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 can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates slide pa ...
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Cinder Cones
A cinder cone (or scoria cone) is a steep conical hill of loose pyroclastic fragments, such as volcanic clinkers, volcanic ash, or scoria that has been built around a volcanic vent. The pyroclastic fragments are formed by explosive eruptions or lava fountains from a single, typically cylindrical, vent. As the gas-charged lava is blown violently into the air, it breaks into small fragments that solidify and fall as either cinders, clinkers, or scoria around the vent to form a cone that often is symmetrical; with slopes between 30 and 40°; and a nearly circular ground plan. Most cinder cones have a bowl-shaped crater at the summit. Mechanics of eruption Cinder cones range in size from tens to hundreds of meters tall and often have a bowl-shaped crater at the summit. They are composed of loose pyroclastic material (cinder or scoria), which distinguishes them from ''spatter cones'', which are composed of agglomerated volcanic bombs. The pyroclastic material making up a cinder ...
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Maars Of Turkey
A maar is a broad, low-relief volcanic crater caused by a phreatomagmatic eruption (an explosion which occurs when groundwater comes into contact with hot lava or magma). A maar characteristically fills with water to form a relatively shallow crater lake which may also be called a maar. The name comes from a Moselle Franconian dialect word used for the circular lakes of the Daun area of Germany. Notes: * According to German Wikipedia's ''"Maar"'' article, in 1544 in his book ''Cosmographia'', Sebastian Münster (1488–1552) first applied the word "maar" (as ''Marh'') to the Ulmener Maar and the Laacher See. See: Sebastian Münster, ''Cosmographia'' (Basel, Switzerland: Heinrich Petri, 1544)p. 341. From p. 341: ''"Item zwen namhafftiger seen seind in der Eyfel / einer bey de schloß Ulmen / und ein ander bey dem Closter züm Laich / die seind sere tieff / habe kein ynflüß aber vil außflüß / die nennet man Marh unnd seind fischreich."'' (Also two noteworthy lakes are ...
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Volcanic Fields
A volcanic field is an area of Earth's crust that is prone to localized volcanic activity. The type and number of volcanoes required to be called a "field" is not well-defined. Volcanic fields usually consist of clusters of up to 100 volcanoes such as cinder cones. Lava flows may also occur. They may occur as a monogenetic volcanic field or a polygenetic volcanic field. Description Alexander von Humboldt observed in 1823 that geologically young volcanoes are not distributed uniformly across the Earth's surface, but tend to be clustered into specific regions. Young volcanoes are rarely found within cratons, but are characteristic of subduction zones, rift zones, or in ocean basins. Intraplate volcanoes are clustered along hotspot traces. Within regions of volcanic activity, volcanic fields are clusters of volcanoes that share a common magma source. Scoria cones are particularly prone to cluster into volcanic fields, which are typically in diameter and consist of several tens ...
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Volcanoes Of Turkey
A volcano is a rupture 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 most 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 can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates slide pa ...
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Meke Gölü Panorama
Meke, in the Fijian language, is all traditional style of dance. It is a cognate of the words ''"maka"'' ( Rotuman) and ''"mele"'' in Hawaiian. It is typically performed during celebrations and festivals. Traditionally the dances that comprise the ''meke'' art form are performed by groups of men only or women only, however, foreign influences, such as the male/female Tongan ma'ulu'ulu becoming the Fijian vakamalolo, are evident throughout. Friedrich Ratzel in his 1896 publication ''The History of Mankind'', writes about the Fijian meke as both song and dance, which only a few are given to invent and which those who do, allege that they do so in the spirit world where divine beings teach them the song and the appropriate dance. He wrote that the ideal of the Fijian poet is poetry with every verse ending with the same vowel of regular measure Measure may refer to: * Measurement, the assignment of a number to a characteristic of an object or event Law * Ballot measure, propose ...
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Diyarbakır
Diyarbakır (; ; ; ) is the largest Kurdish-majority city in Turkey. It is the administrative center of Diyarbakır Province. Situated around a high plateau by the banks of the Tigris river on which stands the historic Diyarbakır Fortress, it is the administrative capital of the Diyarbakır Province of southeastern Turkey. It is the second-largest city in the Southeastern Anatolia Region. As of December 2021, the Metropolitan Province population was 1,791,373 of whom 1,129,218 lived in the built-up (or metro) area made of the 4 urban districts ( Bağlar, Kayapınar, Sur and Yenişehir). Diyarbakır has been a main focal point of the conflict between the Turkish state and various Kurdish separatist groups, and is seen by many Kurds as the de facto capital of Kurdistan. The city was intended to become the capital of an independent Kurdistan following the Treaty of Sèvres, but this was disregarded following subsequent political developments. Names and etymology Th ...
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Karaca Dağ
Karaca Dağ ( ku, قه‌ره‌ژداخ, ) is a shield volcano located in eastern Turkey. It was also known as Mount Masia. Which in turn was used to give the title of an iris found on the mountain, as '' Iris masia''. On 6 March 2006, reported that the Max Planck Institute for Plant Breeding Research in Cologne had discovered that the genetically common ancestor of 68 contemporary types of cereal still grows as a wild plant on the slopes of Mount Karaca (Karacadag). The results strongly suggest that slopes of Karaca Dağ provided the site for the first domestication of einkorn wheat approximately 9,000 years ago. The area of Karaca Dağ was gifted to Ertuğrul Gazi by the Seljuk Sultan of the Sultanate of Rum, Sultan Kayqubad I, after bravely fighting in the Battle of Yassıçemen. See also * 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 Volc ...
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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 ( tr, Türkiye ), officially the Republic of Türkiye ( tr, Türkiye Cumhuriyeti, links=no ), is a transcontinental country located mainly on the Anatolian Peninsula in Western Asia, with a small portion on the Balkan Peninsula in ...
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