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| The state of Opala volcano on 11 September, 2022.
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Date:
11/9/2022
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| Author(s): FEC SRC Planeta |
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| Any use of the image may be carried out only with the permission of the copyright holder |
| © IVS FEB RAS Geoportal |
11/9/2022
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| Opala volcano
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Date:
27/10/2012
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| Author(s): A. Sokorenko, IVS FEB RAS |
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| Any use of the image may be carried out only with the permission of the author (authors) |
| © IVS FEB RAS Geoportal |
27/10/2012
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| Opala volcano.
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Date:
27/10/2012
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| Author(s): A. Sokorenko, IVS FEB RAS |
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| Any use of the image may be carried out only with the permission of the author (authors) |
| © IVS FEB RAS Geoportal |
27/10/2012
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| Map of Location of Opala volcano
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| The map created using Topography and Bathymetry Layers from service: http://www.demis.nl.
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Date:
9/6/2011
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| Author(s): Romanova I.M., IVS FEB RAS |
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| Any use of the image may be carried out only with the permission of the author (authors) |
| © IVS FEB RAS Geoportal |
9/6/2011
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| Opala volcano, view from the east.
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Date:
7/11/2008
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| Author(s): A. Sokorenko, IVS FEB RAS |
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| Any use of the image may be carried out only with the permission of the author (authors) |
| © IVS FEB RAS Geoportal |
7/11/2008
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| Opala volcano, view from the west.
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| Author(s): A. Litsis |
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| Any use of the image may be carried out only with the permission of the author (authors) |
| © IVS FEB RAS Geoportal |
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| Geologic map of Opala volcano
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| Author(s): N.N.Kozhemyaka, A.A.Vazheyevskaya, M.I.Zubin |
| Source: Active Volcanoes of Kamchatka: In 2 vol. Vol. 2. M Nauka, 1991, 415 pp. |
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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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| Opala volcano
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| 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.
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| Author(s): Viktor Dvigalo, IVS FEB RAS |
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| Any use of the image may be carried out only with the permission of the author (authors) |
| © IVS FEB RAS Geoportal |
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