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Kula Volcanic Geopark
Kula Volcanic Geopark, also known as Kula Geopark, ( tr, Kula Volkanik Jeoparkı or ''Kula Jeoparkı'') is a geopark, a protected area of geological heritage, located in Kula, Manisa, western Turkey. It was recognized by UNESCO as a UNESCO Global Geopark in 2013, and is the country's only geopark. Location The volcanic park is located in Manisa Province in western Turkey, covering an area of nearly mainly in Kula district, and stretches in the north into parts of Salihli district. The elevation of the area rises from in Salihli to in Kula. History The volcanic field was first described by the Ancient Greek geographer Strabo (64 or 63 BC – c. 24 AD) in the encyclopedia '' Geographica'', calling it Katakekaumene. The name means "burnt land" or "burnt country", and refers to the pitch-black color of the lava in the dormant volcanic field Kula. The volcanic field attracted many travelers and researchers, including George Keppel (1830), William Hamilton and Hugh Edwin Strick ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kula, Manisa
Kula is a town and district of Manisa Province in the Aegean region of Turkey. According to the 2000 census, population of the district is 52,986 of which 24,217 live in the town of Kula. The district covers an area of , and the town lies at an elevation of . Economy As of 1920, Kula's main industry was carpet making. Yanıkyöre volcanic rock formations The district is renowned for the cone-shaped volcanic rock formations, numbering at about eighty, in the nearby Yanıkyöre (literally ''the burnt land'') area, also sometimes still referred to, including in Turkey, under the Greek name of ''Katakekaumene'', which has the same meaning. Increasingly brought to the attention of a wider public in recent years as a natural curiosity, other recently coined terms to describe the area include "Cappadocia of the Aegean Region, Turkey" or even "Kuladocia". Kula Volcanic Geopark was accepted and certificated by UNESCO The United Nations Educational, Scientific and Cultural Organizat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alfred Philippson
Alfred Philippson (1 January 1864 – 28 March 1953) was a German geologist and geographer. He was born at Bonn, son of Ludwig Philippson. He received his education at the gymnasium and university of his native town and at the University of Leipzig (Ph.D. 1886). In 1892 he became '' Privatdozent'' at Bonn, was appointed assistant professor seven years later, and in 1904 he was called to Bern as professor of geography. Having made voyages through Italy ( Apulia region), Greece, Turkey, and Asia Minor, he published: ''Studien über Wasserscheiden,'' Berlin, 1886; ''Der Peloponnes,'' ib. 1892; ''Europa'' (with Neumann), Leipzig, 1894; ''Thessalien und Epirus,'' Berlin, 1897; ''Beiträge zur Kenntnis der Griechischen Inselwelt,'' Gotha, 1901; ''Das Mittelmeergebiet,'' Leipzig, 1904. He also published essays in the technical journals, such as ''Das fernste Italien. Geographische Reiseskizzen und Studien'', Leipzig, 1925, and ''Apulien'', Netherlands, 1937. Since 1887 Philippson undert ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Viscosity
The viscosity of a fluid is a measure of its resistance to deformation at a given rate. For liquids, it corresponds to the informal concept of "thickness": for example, syrup has a higher viscosity than water. Viscosity quantifies the internal frictional force between adjacent layers of fluid that are in relative motion. For instance, when a viscous fluid is forced through a tube, it flows more quickly near the tube's axis than near its walls. Experiments show that some stress (such as a pressure difference between the two ends of the tube) is needed to sustain the flow. This is because a force is required to overcome the friction between the layers of the fluid which are in relative motion. For a tube with a constant rate of flow, the strength of the compensating force is proportional to the fluid's viscosity. In general, viscosity depends on a fluid's state, such as its temperature, pressure, and rate of deformation. However, the dependence on some of these properties is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lava Flow
Lava is molten or partially molten rock (magma) that has been expelled from the interior of a terrestrial planet (such as Earth) or a moon onto its surface. Lava may be erupted at a volcano or through a fracture in the crust, on land or underwater, usually at temperatures from . The volcanic rock resulting from subsequent cooling is also often called ''lava''. A lava flow is an outpouring of lava during an effusive eruption. (An explosive eruption, by contrast, produces a mixture of volcanic ash and other fragments called tephra, not lava flows.) The viscosity of most lava is about that of ketchup, roughly 10,000 to 100,000 times that of water. Even so, lava can flow great distances before cooling causes it to solidify, because lava exposed to air quickly develops a solid crust that insulates the remaining liquid lava, helping to keep it hot and inviscid enough to continue flowing. The word ''lava'' comes from Italian and is probably derived from the Latin word ''labes'', ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lava Tube
A lava tube, or pyroduct, is a natural conduit formed by flowing lava from a volcanic vent that moves beneath the hardened surface of a lava flow. If lava in the tube empties, it will leave a cave. Formation A lava tube is a type of lava cave formed when a low-viscosity lava flow develops a continuous and hard crust, which thickens and forms a roof above the still-flowing lava stream. Tubes form in one of two ways: either by the crusting over of lava channels, or from pāhoehoe flows where the lava is moving under the surface. Lava usually leaves the point of eruption in channels. These channels tend to stay very hot as their surroundings cool. This means they slowly develop walls around them as the surrounding lava cools and/or as the channel melts its way deeper. These channels can get deep enough to crust over, forming an insulating tube that keeps the lava molten and serves as a conduit for the flowing lava. These types of lava tubes tend to be closer to the lava erupt ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Maar
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scoria Cone
Scoria is a pyroclastic, highly vesicular, dark-colored volcanic rock that was ejected from a volcano as a molten blob and cooled in the air to form discrete grains or clasts.Neuendorf, K.K.E., J.P. Mehl, Jr., and J.A. Jackson, eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. It is typically dark in color (generally dark brown, black or purplish-red), and basaltic or andesitic in composition. Scoria is relatively low in density as a result of its numerous macroscopic ellipsoidal vesicles, but in contrast to pumice, all scoria has a specific gravity greater than 1, and sinks in water. The holes or vesicles form when gases that were dissolved in the magma come out of solution as it erupts, creating bubbles in the molten rock, some of which are frozen in place as the rock cools and solidifies. Scoria may form as part of a lava flow, typically near its surface, or as fragmental ejecta ( lapilli, blocks and bombs), for ins ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kula Volkano
Kula, which translates as ''Tower'' from Serbo-Croatian, may refer to: People *Bob Kula, American football player *Irwin Kula (born 1957), American rabbi and author *Karel Kula (born 1963), Czech footballer Places * Kula, Bihać, a village in Bosnia and Herzegovina * Kula (Bugojno), a village in Bosnia and Herzegovina * Kula, Busovača, a village in Bosnia and Herzegovina * Kula (Konjic), a village in Bosnia and Herzegovina * Kula (Sokolac), a village in Bosnia and Herzegovina * Kula, Travnik, a village in Bosnia and Herzegovina * Kula, Zenica, a village in Bosnia and Herzegovina * Kula, Bulgaria, a town and municipality in Vidin Province, Bulgaria * Kula, Croatia, a village in Požega-Slavonia County, Croatia * Kula, Ethiopia, a town in Ethiopia * Kula Eco Park, a zoological park near Sigatoka, Fiji * Kula, Iran, a village in East Azerbaijan Province, Iran * Kula, Serbia, a town and municipality in Vojvodina, Serbia * Kula (volcano), a volcanic field in Turkey * Kula, Man ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quaternary
The Quaternary ( ) is the current and most recent of the three periods of the Cenozoic Era in the geologic time scale of the International Commission on Stratigraphy (ICS). It follows the Neogene Period and spans from 2.58 million years ago to the present. The Quaternary Period is divided into two epochs: the Pleistocene (2.58 million years ago to 11.7 thousand years ago) and the Holocene (11.7 thousand years ago to today, although a third epoch, the Anthropocene, has been proposed but is not yet officially recognised by the ICS). The Quaternary Period is typically defined by the cyclic growth and decay of continental ice sheets related to the Milankovitch cycles and the associated climate and environmental changes that they caused. Research history In 1759 Giovanni Arduino proposed that the geological strata of northern Italy could be divided into four successive formations or "orders" ( it, quattro ordini). The term "quaternary" was introduced by Jules Desnoye ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanism
Volcanism, vulcanism or volcanicity is the phenomenon of eruption of molten rock (magma) onto the surface of the Earth or a solid-surface planet or moon, where lava, pyroclastics, and volcanic gases erupt through a break in the surface called a vent. It includes all phenomena resulting from and causing magma within the crust or mantle of the body, to rise through the crust and form volcanic rocks on the surface. Magmas, that reach the surface and solidify, form extrusive landforms. Volcanic processes Magma from the mantle or lower crust rises through the crust towards the surface. If magma reaches the surface, its behavior depends on the viscosity of the molten constituent rock. Viscous (thick) magma produces volcanoes characterised by explosive eruptions, while non-viscous (runny) magma produce volcanoes characterised by effusive eruptions pouring large amounts of lava onto the surface. In some cases, rising magma can cool and solidify without reaching the surface. Inste ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aegean Region
The Aegean Region () is one of the 7 Geographical regions of Turkey, geographical regions of Turkey. The largest city in the region is İzmir. Other big cities are Manisa, Aydın, Denizli, Muğla, Afyonkarahisar and Kütahya. Located in western Turkey, it is bordered by the Aegean Sea to the west, the Marmara Region to the north, the Central Anatolia Region to the east, and the Mediterranean Region, Turkey, Mediterranean Region to the south. Among the four coastal regions, the Aegean Region has the longest coastline. Subdivision *Aegean Section ( tr, Ege Bölümü) **Edremit Area ( tr, Edremit Yöresi) **Bakırçay Area ( tr, Bakırçay Yöresi) **Gediz Area ( tr, Gediz Yöresi) **İzmir Area ( tr, İzmir Yöresi) **Küçük Menderes Area ( tr, Küçük Menderes Yöresi) **Büyük Menderes Area ( tr, Büyük Menderes Yöresi) **Menteşe Area ( tr, Menteşe Yöresi) * Inner Western Anatolia Section ( tr, İç Batı Anadolu Bölümü) Ecoregions The ecoregions of this ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tectonics
Tectonics (; ) are the processes that control the structure and properties of the Earth's crust and its evolution through time. These include the processes of mountain building, the growth and behavior of the strong, old cores of continents known as cratons, and the ways in which the relatively rigid plates that constitute the Earth's outer shell interact with each other. Tectonics also provide a framework for understanding the earthquake and volcanic belts that directly affect much of the global population. Tectonic studies are important as guides for economic geologists searching for fossil fuels and ore deposits of metallic and nonmetallic resources. An understanding of tectonic principles is essential to geomorphologists to explain erosion patterns and other Earth surface features. Main types of tectonic regime Extensional tectonics Extensional tectonics is associated with the stretching and thinning of the crust or the lithosphere. This type of tectonics is found ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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