|
|
| Pages:
1 |
-
| O
|
Date:
27/10/2012
|
| |
| Author(s): A. Sokorenko, IVS FEB RAS |
| |
| Any use of the image may be carried out only with the permission of the author (authors) |
| © IVS FEB RAS Geoportal |
27/10/2012
-
| O
|
Date:
27/10/2012
|
| |
| Author(s): A. Sokorenko, IVS FEB RAS |
| |
| Any use of the image may be carried out only with the permission of the author (authors) |
| © IVS FEB RAS Geoportal |
27/10/2012
-
| O
|
Date:
7/11/2008
|
| |
| Author(s): A. Sokorenko, IVS FEB RAS |
| |
| Any use of the image may be carried out only with the permission of the author (authors) |
| © IVS FEB RAS Geoportal |
7/11/2008
-
| O
|
| |
| Author(s): A. Litsis |
| |
| Any use of the image may be carried out only with the permission of the author (authors) |
| © IVS FEB RAS Geoportal |
-
| O
|
| This is probably the best picture of Opala volcano, taken from ESE. The volcano sits on the northern rim of a large Late Pleistocene caldera (a part of the rim is seen in the low right corner of the picture). Opala is a hystorically active volcano; its last large eruption occurred about 300 years ago. Baranii Amphitheater crater, filled with extrusive domes, is at the foreground. It formed about 1500 years BP and produced 9-10 km3 of rhyolitic tephra.
|
| |
| Author(s): Viktor Dvigalo, IVS FEB RAS |
| |
| Any use of the image may be carried out only with the permission of the author (authors) |
| © IVS FEB RAS Geoportal |
|
|
Images since 1 to 5 of 5 |
|
|
|
