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Titila shield volcano viewed from the south
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Titila started to form in the late Pleistocene time. The volcano was active 10-8 and 3-2.5 ka BP (14C) (Dirksen et al., 2003, 2004). A flank vent (a summit in front of Titila) was formed in early Holocene. Its lava flows dammed a river to form Glubokoe ("Deep") Lake (at the far right). Titila eruptives are transitional from medium to high-K basalt.
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Author(s): Maxim Portnyagin |
Source: IVS FEB RAS. Holocene Kamchatka Volcanoes http://www.kscnet.ru/ivs/volcanoes/holocene/ |
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Any use of the image may be carried out only with the permission of the author (authors). Please cite the author(s) and the Geoportal when using this image. |
© IVS FEB RAS Geoportal |
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