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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.

Gerçek volkan patlaması

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Gerçek volkan patlaması

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Turkish Journal of Earth Sci- ence, 16, Yerbilimleri, vol. Rapa Nui Journal. The morphology and formation of flow-lobe tumuli on Icelandic shield volcanoes. British Battles Mount Badon to Brunanburh. Tephra volumes and erupted masses". Levy, David ed. Riedel, C. Dumbarton Oaks Papers. The total erupted volume VT is estimated as 3. Prentice- Hall, Englewood Cliffs, N. Journal of Geophysical Research. Lava flow in tubes with elliptical cross sections.

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Geodinamica Acta, 16, Constraints on the timing and regional conditions at the start of the presence phase of crustal extension in western Turkey, from observations in and around the Denizli region. Israel Journal of Earth Science, 44, Prentice- Hall, Englewood Cliffs, N. Volcanic Successions. International Journal of Earth Sciences, 89, Geometry and origin of folding in the Neogene sediments of the Gediz Graben, western Anatolia, Turkey. Studies of Geophysics. The North Anatolian Fault Zone. Quaternary Research. Geology, 29, Turkish Journal of Earth Science, 5, Distribution, morphology, and size frequency of cinder cones on Mauna Kea volcano, Hawaii. Gonnermann, H.