About koh-e-sultan

Koh-i-Sultan is a volcano in Balochistan, Pakistan. It is a part of the tectonic belt shaped via way of means of the collision of India and Asia: specifically, a section encouraged via way of means of the subduction of the Arabian plate below the Asian plate and forming a volcanic arc that incorporates the Bazman and Taftan volcanoes in Iran. The volcano includes 3 predominant cones, with closely eroded craters walking west-northwest and surrounded via way of means by some subsidiary volcanic centers. Its summit is 2,334 meters (7,657 ft) high, and the crater related to the Miri cone has a smaller crater inside. The volcano is shaped via way of means of andesite and dacite rocks, with fragmentary rocks winning over lava flows. The rocks have common arc-volcano chemistry and composition, with development from andesite to dacite withinside the eruption merchandise with more youthful age. Potassium-argon relationship has indicated an age variety from 5,900,000 to 90,000 years. Subsequent erosion has generated a big particles apron across the base of the volcano and carved rock formations that inspired early explorers; one famous rock formation is Neza e Sultan. Geothermal interest and the emission of volcanic gases are ongoing, and the volcano has prospected for the opportunity of acquiring geothermal energy. The geothermal interest has led to extensive rock alteration and the formation of sulfur deposits, which have been noted in a 1909 document and later mined. Koh-i-Sultan additionally has deposits of different minerals.

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