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Tarso Ahon

Tarso Ahon is a Pleistocene volcano in Tibesti, north of Emi Koussi[1] from which it is separated by deep gorges.[2] It covers a surface of about 50 by 60 kilometres (31 mi × 37 mi)[3] and is a so-called volcanic plateau[4] with three summits: Arken Ahon, Dondomé, Tarso Ahon and Tarso Mohi. However, contrary to its plateau-like appearance the basaltic surfaces of Tarso Ahon are difficult to access and steep. Tarso Ahon has erupted andesite, rhyolite and similar magmas, and more recently basalts which form lava flows.[5]

Tarso Ahon
Tarso Ahon
Highest point
Elevation3,325 m (10,909 ft)[1]
Coordinates20°32′20″N 18°17′24″E / 20.539°N 18.29°E / 20.539; 18.29[1]

References edit

  1. ^ a b c "Tarso Ahon". Global Volcanism Program. Smithsonian Institution.
  2. ^ Gèze et al. 1959, p. 138.
  3. ^ Permenter & Oppenheimer 2007, p. 615.
  4. ^ Permenter & Oppenheimer 2007, p. 618.
  5. ^ Gèze et al. 1959, p. 140.

Sources edit

  • Gèze, B.; Hudeley, H.; Vincent, P.; Wacrenier, Ph (1 December 1959). "Les volcans du Tibesti (Sahara du Tchad)". Bulletin Volcanologique (in French). 22 (1): 135–172. Bibcode:1959BVol...22..135G. doi:10.1007/BF02596582. ISSN 0366-483X. S2CID 128896369.
  • Permenter, Jason L.; Oppenheimer, Clive (1 April 2007). "Volcanoes of the Tibesti massif (Chad, northern Africa)". Bulletin of Volcanology. 69 (6): 609–626. Bibcode:2007BVol...69..609P. doi:10.1007/s00445-006-0098-x. ISSN 0258-8900. S2CID 53463999.

tarso, ahon, pleistocene, volcano, tibesti, north, koussi, from, which, separated, deep, gorges, covers, surface, about, kilometres, called, volcanic, plateau, with, three, summits, arken, ahon, dondomé, tarso, mohi, however, contrary, plateau, like, appearanc. Tarso Ahon is a Pleistocene volcano in Tibesti north of Emi Koussi 1 from which it is separated by deep gorges 2 It covers a surface of about 50 by 60 kilometres 31 mi 37 mi 3 and is a so called volcanic plateau 4 with three summits Arken Ahon Dondome Tarso Ahon and Tarso Mohi However contrary to its plateau like appearance the basaltic surfaces of Tarso Ahon are difficult to access and steep Tarso Ahon has erupted andesite rhyolite and similar magmas and more recently basalts which form lava flows 5 Tarso AhonTarso AhonHighest pointElevation3 325 m 10 909 ft 1 Coordinates20 32 20 N 18 17 24 E 20 539 N 18 29 E 20 539 18 29 1 References edit a b c Tarso Ahon Global Volcanism Program Smithsonian Institution Geze et al 1959 p 138 Permenter amp Oppenheimer 2007 p 615 Permenter amp Oppenheimer 2007 p 618 Geze et al 1959 p 140 Sources edit Geze B Hudeley H Vincent P Wacrenier Ph 1 December 1959 Les volcans du Tibesti Sahara du Tchad Bulletin Volcanologique in French 22 1 135 172 Bibcode 1959BVol 22 135G doi 10 1007 BF02596582 ISSN 0366 483X S2CID 128896369 Permenter Jason L Oppenheimer Clive 1 April 2007 Volcanoes of the Tibesti massif Chad northern Africa Bulletin of Volcanology 69 6 609 626 Bibcode 2007BVol 69 609P doi 10 1007 s00445 006 0098 x ISSN 0258 8900 S2CID 53463999 nbsp This volcanology article is a stub You can help Wikipedia by expanding it vte nbsp This Chad location article is a stub You can help Wikipedia by expanding it vte Retrieved from https en wikipedia org w index php title Tarso Ahon amp oldid 1007982398, wikipedia, wiki, book, books, library,

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