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Vsevidof volcano

Stratovolcano 2149 m / 7,050 ft
United States, Aleutian Islands, 53.13°N / -168.69°W
Current status: dormant (1 out of 5) | Reports
Vsevidof volcano books
Typical eruption style: unspecified
Vsevidof volcano eruptions: 1878  No recent earthquakes
TimeMag. / DepthDistanceLocation

Background:

The symmetrical Vsevidof stratovolcano, near the SW end of Umnak Island, is one of the most prominent volcanoes in the Aleutians. Vsevidof contains a 1.2-km-wide, ice-filled summit crater that is breached by glaciers on the east and north sides. An E-W-trending zone of scoria cones that extends from 1220 m down much of the western flank has been the source of historical eruptions. The bulk of the 2149-m-high cone of Vsevidof was constructed during the Holocene. Young andesitic and dacitic lava flows were extruded from vents on the north and south flanks and on the west-flank rift. The largest lava flow traveled down the west flank to the coast, forming Cape Kigushimkada.
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Smithsonian / GVP volcano information


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