Mount Vsevidof
Vsevidof
Stratovolkan · United States · 2160 m

- Tipe
- Stratovolkan
- Negara
- United States
- Wilayah
- North America Volcanic Regions / Aleutian Ridge Volcanic Arc
- Ketinggian
- 2160 m
- Koordinat
- 53.126, -168.688
- Letusan terakhir
- 1878
- Kondisi tektonik
- Subduction zone / Intermediate crust (15-25 km)
- Bentuk lahan
- Composite
- Batuan utama
- Andesite / Basaltic Andesite
Ringkasan geologi
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.
Riwayat letusan
Ringkasan (VEI dari waktu ke waktu)
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Garis waktu rinci
- 1957VEI 2Perkiraan geologi1957-03-11 – 1957-03-12West flank fissure
- 1880VEI ?Perkiraan geologi1880 – Berlangsung
- 1878VEI 2Teramati1878 – BerlangsungWest flank fissure ?
- 1830VEI ?Teramati1830 – BerlangsungSW end of Umnak Island
- 1817VEI 3Teramati1817 – Berlangsung
- 1790VEI ?Perkiraan geologi1790-05-30 – Berlangsung
- 1784VEI ?Perkiraan geologi1784 – Berlangsung
Tautan eksternal
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