|
|
| Pages:
1 |
-
| Titila shield volcano viewed from the south
|
| 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.
|
| |
| Author(s): Maxim Portnyagin |
| Source: IVS FEB RAS. Holocene Kamchatka Volcanoes http://www.kscnet.ru/ivs/volcanoes/holocene/ |
| |
| 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 |
|
|
Images since 1 to 1 of 1 |
|
|
|
