Ostry вулкан

Справочная информация:

Conical Ostry volcano, its slopes partially mantled by glaciers, is a late-Quaternary stratovolcano that rises to 2552 m, forming one of the highest peaks of the northern Sredinny Range. Ostry, also known as Ostraya, is located on the western side of the major NE-trending graben along the axis of the northern Sredinny Range. An unnamed 2127-m-high cinder cone on the SW flank of Ostry, informally referred to as "Cone X," erupted about 4000 years ago, producing a basaltic lava flow.
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Smithsonian / GVP volcano information

Ostry Фото:

The Tolbachik volcano massif seen in the evening blue hour from our campsite. To the left, the active Plosky (flat) Tolbachik (3,085 m), a very active shield volcano, and...	Ostry and Plosky Tolbachik ("pointed" and "flat") seen when reaching the vast lapilli fields on the southern rift zone. (Photo: Tom Pfeiffer)	View to Plosky (l) and Ostry (r) Tolbachik volcanoes from a little cinder cone near the campsite. (Photo: Tom Pfeiffer)
Ostry Tolbachik, Plosky Tolbachik, and Zimina volcanoes with cinder cones in the foreground. (Photo: Tom Pfeiffer)	Ostry Tolbachik is the remnant of an older steep-sides stratovolcano, which has collapsed some 6500 years ago towards the south. (Photo: Tom Pfeiffer)	About one hour to go, the cone of Ostry Tolbachik becomes sometimes visible from the road. (Photo: Tom Pfeiffer)

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See also: Sentinel hub | Landsat 8