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dc.contributor.author Edwards B. en
dc.contributor.author Belousov A. en
dc.contributor.author Belousova M. en
dc.contributor.author Volynets A. en
dc.contributor.author Melnikov D. en
dc.contributor.author Chirkov S. en
dc.contributor.author Senyukov S. en
dc.contributor.author Gordeev E. en
dc.contributor.author Muraviev Y. en
dc.contributor.author Izbekov P. en
dc.contributor.author Demianchuk Y. en
dc.date.accessioned 2019-03-04T02:01:14Z
dc.date.available 2019-03-04T02:01:14Z
dc.date.issued 2013
dc.identifier.citation Eos, Vol. 94, No. 21, 21 May 2013, 189–191 en
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/1485
dc.description.abstract On 27 November 2012 at 1715 local time, a focused swarm of earthquakes was interpreted as the start of a new ongoing eruption on the south flank (Tolbachinsky Dol) of Plosky Tolbachik volcano in east central Kamchatka, Russia (Figure 1a) [Samoylenko et al., 2012]. Visual observations on 29 November showed ash shooting from two fractures as well as long, rapidly moving lava flows. Although the initial ash clouds reached 6 kilometers in height, subsequent ashfall has been limited to the area around the main vents, and no permanent settlements are in danger from advancing lava flows (the closest settlements are about 40 kilometers from the volcano). Including this eruption, six different volcanoes are presently active in Kamchatka. en
dc.language Английский ru_RU
dc.subject 38.37.25 Вулканология ru_RU
dc.subject Плоский Толбачик ru_RU
dc.title ANOTHER “GREAT TOLBACHIK” ERUPTION? en
dc.type Статья, тезисы доклада ru_RU


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