| dbo:abstract |
Koh-i-Sultan is a volcano in Balochistan, Pakistan. It is part of the tectonic belt formed by the collision of India and Asia: specifically, a segment influenced by the subduction of the Arabian plate beneath the Asian plate and forming a volcanic arc which includes the Bazman and Taftan volcanoes in Iran. The volcano consists of three main cones, with heavily eroded craters running west-northwest and surrounded by a number of subsidiary volcanic centres. Its summit is 2,334 metres (7,657 ft) high, and the crater associated with the Miri cone has a smaller crater inside. The volcano is formed by andesite and dacite rocks, with fragmentary rocks prevailing over lava flows. The rocks have typical arc-volcano chemistry and composition, with a progression from andesite to dacite in the eruption products with younger age. Potassium-argon dating has indicated an age range from 5,900,000 to 90,000 years. Subsequent erosion has generated a large debris apron around the base of the volcano and carved rock formations which impressed early explorers; one well-known rock formation is Neza e Sultan. Geothermal activity and the emission of volcanic gases are ongoing, and the volcano has been prospected for the possibility of obtaining geothermal energy. The geothermal activity has resulted in widespread rock alteration and the formation of sulfur deposits, which were mentioned in a 1909 report and later mined. Koh-i-Sultan also has deposits of other minerals. (en) Koh-i-Sultan es un estratovolcán extinto de la era del Pleistoceno en el cinturón magmático Chagai de Baluchistán, Pakistán. El volcán se caracteriza por una caldera, que ha sido objeto de exploraciones minerales recientes. Depósitos de azufre se pueden encontrar en el lado sur del volcán, así como manantiales de agua caliente alrededor del cráter de Miri. Hay dos picos, Koh-i-Sultán del Este, a 2030 metros, y Koh-i-Sultán del Oeste, a 2340 metros. (es) |
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Koh-e-Sultan, Kuh-i-Sultan, Kuh-e-Sultan (en) |
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dbr:Stratovolcano |
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https://books.google.com/books%3Fid=Li_XoQEACAAJ%7Cyear=1973%7Cpublisher=Geological https://pubs.er.usgs.gov/publication/ofr75496%7Cwebsite=pubs.usgs.gov%7Cpublisher=USGS https://pubs.er.usgs.gov/publication/ofr75550%7Cwebsite=USGS https://zenodo.org/record/2452264%7Cref=none http://digitalcommons.unomaha.edu/cgi/viewcontent.cgi%3Farticle=1043&context=afghanuno%7Cwebsite=digitalcommons.unomaha.edu%7Cpublisher=B http://nceg.uop.edu.pk/GeologicalBulletin/Vol-42-2009/Vol-42-2009-Paper1.pdf%7Caccess-date=31 http://dro.dur.ac.uk/12675/1/12675.pdf%7Cref=none https://inis.iaea.org/search/search.aspx%3Forig_q=RN:41078859%7Cwebsite= |
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dbr:Miocene dbr:Late_Pleistocene |
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3.15576E11 (dbd:second) |
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Koh-i-Sultan is located in westernmost Pakistan (en) |
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Koh-i-Sultan (en) |
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Koh-e-Sultan, Kuh-i-Sultan, Kuh-e-Sultan (en) |
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Mountain of the King (en) |
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dbr:Stratovolcano |
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Sultan/Makran/Baluchistan volcanic arc (en) |
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| rdfs:comment |
Koh-i-Sultan es un estratovolcán extinto de la era del Pleistoceno en el cinturón magmático Chagai de Baluchistán, Pakistán. El volcán se caracteriza por una caldera, que ha sido objeto de exploraciones minerales recientes. Depósitos de azufre se pueden encontrar en el lado sur del volcán, así como manantiales de agua caliente alrededor del cráter de Miri. Hay dos picos, Koh-i-Sultán del Este, a 2030 metros, y Koh-i-Sultán del Oeste, a 2340 metros. (es) Koh-i-Sultan is a volcano in Balochistan, Pakistan. It is part of the tectonic belt formed by the collision of India and Asia: specifically, a segment influenced by the subduction of the Arabian plate beneath the Asian plate and forming a volcanic arc which includes the Bazman and Taftan volcanoes in Iran. The volcano consists of three main cones, with heavily eroded craters running west-northwest and surrounded by a number of subsidiary volcanic centres. Its summit is 2,334 metres (7,657 ft) high, and the crater associated with the Miri cone has a smaller crater inside. (en) |
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Koh-i-Sultan (es) Koh-i-Sultan (en) |
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