Mount Hasan
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Mount Hasan
Mount Hasan ( tr, Hasan Dağı) is a volcano in Anatolia, Turkey. It has two summits, the high eastern Small Hasan Dagi and the high Big Hasan Dagi, and rises about above the surrounding terrain. It consists of various volcanic deposits, including several calderas, and its activity has been related to the presence of several faults in the area and to regional tectonics. Activity began in the Miocene and continued into the Holocene; a mural found in the archeological site of Çatalhöyük have been controversially interpreted as showing a volcanic eruption or even a primitive map. It was the second mountain from the south in the Byzantine beacon system used to warn the Byzantine capital of Constantinople of incursions during the Arab–Byzantine wars. Etymology The modern name of Mount Hasan is widely accepted to be in dedication to Ebu'l-Gazi (El-Hasan), brother of Ebu'l-Kasım during the reign of the Anatolian Seljuks. It is hypothesized that Mount Hasan’s name was ...
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Ultra Prominent Peak
An ultra-prominent peak, or Ultra for short, is a mountain summit with a topographic prominence of or more; it is also called a P1500. The prominence of a peak is the minimum height of climb to the summit on any route from a higher peak, or from sea level if there is no higher peak. There are approximately 1,524 such peaks on Earth. Some well-known peaks, such as the Matterhorn and Eiger, are not Ultras because they are connected to higher mountains by high cols and therefore do not achieve enough topographic prominence. The term "Ultra" originated with earth scientist Steve Fry, from his studies of the prominence of peaks in Washington in the 1980s. His original term was "ultra major mountain", referring to peaks with at least of prominence. Distribution Currently, 1,518 Ultras have been identified above sea level: 639 in Asia, 356 in North America, 209 in South America, 120 in Europe (including 12 in the Caucasus), 84 in Africa, 69 in Oceania, and 41 in Antarctica. ...
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Mount Erciyes
Mount Erciyes ( tr, Erciyes Dağı), also known as Argaeus (Greek: ) is a volcano in Turkey. It is a large stratovolcano surrounded by many monogenetic vents and lava domes, and one maar. The bulk of the volcano is formed by lava flows of andesitic and dacitic composition. At some time in the past, part of the summit collapsed towards the east. The volcano began to form in the Miocene. At first, a volcano farther east named formed from lava flows. Then, again to the east, large explosive eruptions formed a caldera. During the Pleistocene, Mount Erciyes proper grew inside the caldera together with a group of lava domes. Lateral eruptions of Erciyes may have generated ash layers in the Black Sea and the Mediterranean during the early Holocene. The last eruptions occurred during the early Holocene and may have deposited ash as far away as Palestine; the occurrence of historical volcanism is uncertain. Future eruptions of Erciyes may endanger the nearby cities to the north. Th ...
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Monogenetic Volcanic Field
A monogenetic volcanic field is a type of volcanic field consisting of a group of small monogenetic volcanoes, each of which erupts only once, as opposed to polygenetic volcanoes, which erupt repeatedly over a period of time. The small monogenetic volcanoes of these fields are the most common subaerial volcanic landform. Many monogenetic volcanoes are cinder cones, often with lava flows, such as Parícutin in the Michoacán-Guanajuato volcanic field, which erupted from 1943 to 1952. Some monogenetic volcanoes are small lava shields, such as Rangitoto Island in the Auckland volcanic field. Other monogenetic volcanoes are tuff rings or maars. A monogenetic field typically contains between ten and a hundred volcanoes. The Michoacán-Guanajuato field in Mexico contains more than a thousand volcanoes and is exceptionally large. Monogenetic fields occur only where the magma supply to the volcano is low or where vents are not close enough or large enough to develop plumbing system ...
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Ignimbrite
Ignimbrite is a type of volcanic rock, consisting of hardened tuff. Ignimbrites form from the deposits of pyroclastic flows, which are a hot suspension of particles and gases flowing rapidly from a volcano, driven by being denser than the surrounding atmosphere. New Zealand geologist Patrick Marshall (1869-1950) coined the term ''ignimbrite'' from the Latin ''igni-'' ireand ''imbri-'' ain Ignimbrites are made of a very poorly sorted mixture of volcanic ash (or tuff when lithified) and pumice lapilli, commonly with scattered lithic fragments. The ash is composed of glass shards and crystal fragments. Ignimbrites may be loose and unconsolidated, or lithified (solidified) rock called lapilli-tuff. Near the volcanic source, ignimbrites often contain thick accumulations of lithic blocks, and distally, many show meter-thick accumulations of rounded cobbles of pumice. Ignimbrites may be white, grey, pink, beige, brown, or black depending on their composition and density. Many pale ...
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Cappadocian
Cappadocian Greeks also known as Greek Cappadocians ( el, Έλληνες-Καππαδόκες, Ελληνοκαππαδόκες, Καππαδόκες; tr, Kapadokyalı Rumlar) or simply Cappadocians are an ethnic Greek community native to the geographical region of Cappadocia in central-eastern Anatolia, roughly the Nevşehir Province and surrounding provinces of modern Turkey. There had been a continuous Greek presence in Cappadocia since antiquity, and the indigenous populations of Cappadocia, some of whose Indo-European languages may have been closely related to Greek, (cf. Phrygian) became entirely Greek-speaking by at least the 5th century. In the 11th century Seljuq Turks arriving from Central Asia conquered the region, beginning its gradual shift in language and religion. According to 1897 estimations, the sanjak of Konya had a total Greek population of 68,101 and according to Ottoman population statistics of 1914, the sanjak of Niğde had a total Greek population of 5 ...
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Pasture
Pasture (from the Latin ''pastus'', past participle of ''pascere'', "to feed") is land used for grazing. Pasture lands in the narrow sense are enclosed tracts of farmland, grazed by domesticated livestock, such as horses, cattle, sheep, or swine. The vegetation of tended pasture, forage, consists mainly of grasses, with an interspersion of legumes and other forbs (non-grass herbaceous plants). Pasture is typically grazed throughout the summer, in contrast to meadow which is ungrazed or used for grazing only after being mown to make hay for animal fodder. Pasture in a wider sense additionally includes rangelands, other unenclosed pastoral systems, and land types used by wild animals for grazing or browsing. Pasture lands in the narrow sense are distinguished from rangelands by being managed through more intensive agricultural practices of seeding, irrigation, and the use of fertilizers, while rangelands grow primarily native vegetation, managed with extensive practic ...
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Taşpınar, Aksaray
Taşpınar is a town (''belde'') and municipality in the Aksaray District, Aksaray Province, Turkey. Its population is 2,759 (2021). Geography Taşpınar is in the Anatolian plateau, just west of Mount Hasan. The average altitude is . History The earliest residents of the village were the members of a tribe from Azerbaijan in 1515. Eventually, people from nearby villages also settled in Taşpınar. Meanwhile, a group of Taşpınar residents chose to live in Hotamış, another town roughly south west of Taşpınar. In 1957 Taşpınar was declared a seat of township. Economy The main economic activity is handmade rugs. Taşpınar rugs are especially famous for their high density of knots. (40·40 in 10 cm² or more in older rugs.)Aksaray governor’s page
Although the town is situated in a volcanic plateau which is ...
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Helvadere
Helvadere is a town ('' belde'') and municipality in the Aksaray District, Aksaray Province, Turkey. Its population is 2,564 (2021). Geography Helvadere is on the western slopes of Mount Hasan at about . It is south of Aksaray. History Helvadere is situated next to ruins of the ancient town Nora, which was an important town in Hellenistic Capadocia. Eventually, the town lost its former importance and in the Middle Ages it was a small village named Hardaldere. Evliya Çelebi in his Seyahatname describes hardaldere as a village of 65 houses; the majority of the population being Turk Turk or Turks may refer to: Communities and ethnic groups * Turkic peoples, a collection of ethnic groups who speak Turkic languages * Turkish people, or the Turks, a Turkic ethnic group and nation * Turkish citizen, a citizen of the Republic o ..., but also with a Greek minority. In the early 20th century, the name was Halvadara. But in 1968 Halvadara was declared a town nam ...
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Aksaray
Aksaray (, Koine Greek: Ἀρχελαΐς ''Arhelays'', Medieval Greek: Κολώνεια ''Koloneya'', Ancient Greek: Γαρσάουρα ''Garsaura'') is a city in the Central Anatolia region of Turkey and the capital of Aksaray Province. In 2020 the province had an estimated population of 423,011 distributed over about . The average elevation is , with the highest point being Mt. Hasan (Turkish: ''Hasan Dağı'') at . The city of Aksaray has a long history and was an important stopover point on the Silk Road that transited Anatolia for centuries. It is a pleasant small city with the Melendiz river running through it and several monuments dating back to the pre-Ottoman era as well as some impressive examples of government buildings from the early Turkish Republic that are gathered around the main square. The nearest airport is Kapadokya Nevşehir Airport (NAV) which is 62.1 km away from the city. Etymology In antiquity the area was named ''Archelais Garsaura'', which was m ...
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Pontic Mountains
The Pontic Mountains or Pontic Alps (Turkish: ''Kuzey Anadolu Dağları'', meaning North Anatolian Mountains) form a mountain range in northern Anatolia, Turkey. They are also known as the ''Parhar Mountains'' in the local Turkish and Pontic Greek languages. The term ''Parhar'' originates from a Hittite word meaning "high" or "summit". In ancient Greek, the mountains were called the Paryadres or Parihedri Mountains. Geography The range runs roughly east–west, parallel and close to the southern coast of the Black Sea. It extends northeast into Georgia, and west into the Sea of Marmara, with the northwestern spur of the Küre Mountains (and their western extension the Akçakoca Mountains) and the Bolu Mountains, following the coast. The highest peak in the range is Kaçkar Dağı, which rises to . The North Anatolian Fault and the Northeast Anatolian Fault, which are east–west-running strike-slip faults, run along the length of the range. Ecology The mountains are genera ...
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