Mount Vsevidof
Vsevidof
Stratovolcano · United States · 2160m

- Type
- Stratovolcano
- Country
- United States
- Region
- North America Volcanic Regions / Aleutian Ridge Volcanic Arc
- Elevation
- 2160m
- Coordinates
- 53.126, -168.688
- Last eruption
- 1878
- Tectonic setting
- Subduction zone / Intermediate crust (15-25 km)
- Landform
- Composite
- Major rock type
- Andesite / Basaltic Andesite
Geological summary
The symmetrical Vsevidof stratovolcano, near the SW end of Umnak Island, contains a 1.2-km-wide, ice-filled summit crater that is breached by glaciers on the E and N sides. An E-W-trending zone of scoria cones that extends down much of the W flank has been the source of recorded eruptions. Most of the cone was constructed during the Holocene. Andesitic and dacitic lava flows originated from vents on the N and S flanks, and on the W-flank rift. The largest lava flow traveled down the W flank to the coast, forming Cape Kigushimkada.
Eruption history
Summary (VEI over time)
Click a bar to see individual eruptions
Detailed timeline
- 1957VEI 2Geological estimate1957-03-11 – 1957-03-12West flank fissure
- 1880VEI ?Geological estimate1880 – Ongoing
- 1878VEI 2Observed1878 – OngoingWest flank fissure ?
- 1830VEI ?Observed1830 – OngoingSW end of Umnak Island
- 1817VEI 3Observed1817 – Ongoing
- 1790VEI ?Geological estimate1790-05-30 – Ongoing
- 1784VEI ?Geological estimate1784 – Ongoing
External links
⚠ For reference only. Not for emergency response.