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The KVF consists of 80 cinder cones, 5 maars, 8 spatter cones and 6 tumuli. The volcanic products of KVF are alkaline in character and classified as basanite and phonotephrite according to chemical compositions. The dominant mineralogical assemblage in basaltic lavas is comprised of clinopyroxene, olivine, hornblende for B-II and B-III stage , plagioclase and feldspathoids. The volume of the pyroclastic deposits is estimated by detailed morphological investigations in the field as well as by using the topographic maps. Cinder cones have a median basal diameter Wco of m, a median height Hco of 45 m, and a median volume VC of 5. The total erupted volume VT is estimated as 3. The total ejecta volume VE and total juvenile component volume VJ are estimated to be 0.

Gerçek volkan patlaması

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Levy, David ed. Quaternary Science Reviews. Turkish Journal of Earth Sci- ence, 16,

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Climate : the force that shapes our world and the future of life on earth. Londra: Rodale Books International. Dumbarton Oaks Papers. Modern and Ancient. Volcanic rift zones and their intrusion swarms. Hanson, S. Journal of Volcanology and Geothermal Research, 94, Origin of NE-trending basins in western Turkey. Keszthelyi, L. Kategori : 6. High-pressure metamorphism in the Aegean, eastern Mediterranean: underplating and exhu- mation from the Late Cretaceous until the Miocene and Recent above the ret- reating Hellenic subduction zone. Belgesel, Felaket! The cinder cones of Michoacan-Guana- juato, Central Mexico: their age, volume and distribution, and magma discharge rate.

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Bente Magnus Ed. Bozkurt, E. Physics of thermohydraulic explosions. Ge- odinamica Acta, 18, The Holocene. Economic Geology, 90, London, England: William Heinemann. British Battles Mount Badon to Brunanburh. Aubele ,J. Origin of NE-trending basins in western Turkey.