Semisopochnoi Island
Semisopochnoi
Stratovolcano · United States · 1221m

- Type
- Stratovolcano
- Country
- United States
- Region
- North America Volcanic Regions / Aleutian Ridge Volcanic Arc
- Elevation
- 1221m
- Coordinates
- 51.930, 179.580
- Last eruption
- 2023
- Tectonic setting
- Subduction zone / Intermediate crust (15-25 km)
- Landform
- Composite
- Major rock type
- Basalt / Picro-Basalt
Geological summary
Semisopochnoi, the largest subaerial volcano of the western Aleutians, is 20 km wide at sea level and contains an 8-km-wide caldera. It formed as a result of collapse of a low-angle, dominantly basaltic volcano following the eruption of a large volume of dacitic pumice. The high point of the island is Anvil Peak, a double-peaked late-Pleistocene cone that forms much of the island's northern part. The three-peaked Mount Cerberus (renamed Mount Young in 2023) was constructed within the caldera during the Holocene. Each of the peaks contains a summit crater; lava flows on the N flank appear younger than those on the south side. Other post-caldera volcanoes include the symmetrical Sugarloaf Peak SSE of the caldera and Lakeshore Cone, a small cinder cone at the edge of Fenner Lake in the NE part of the caldera. Most documented eruptions have originated from Young, although Coats (1950) considered that both Sugarloaf and Lakeshore Cone could have been recently active.
From Wikipedia
Semisopochnoi Island or Unyak Island is part of the Rat Islands group in the western Aleutian Islands of Alaska. The island is uninhabited and provides an important nesting area for maritime birds. The island is of volcanic origin, containing several volcanoes including Mount Young. It has a land area of 85.558 square miles, measuring 11 miles (18 km) in length and 12 miles (20 km) in width.
Wikipedia · CC BY-SA · Read full article →
Eruption history
Detailed timeline
- 2021VEI 2Observed2021-02-02 – 2023-05-05North Cerberus
- 2019VEI 1Observed2019-12-07 – 2020-06-19North Cerberus
- 2019VEI 1Observed2019-07-16 – 2019-08-24
- 2018VEI 1Observed2018-09-08 – 2018-10-31North Cone of Mount Cerberus (Mount Young)
- 1987VEI 2Observed1987-04-13 – 1987-04-18Sugarloaf ?
- 1873VEI ?Observed1873 – OngoingCerberus
- 1830VEI ?Geological estimate1830 – OngoingCerberus
- 1792VEI ?Geological estimate1792 – OngoingCerberus
- 1790VEI ?Geological estimate1790 – OngoingCerberus
- 1772VEI ?Geological estimate1772 – OngoingCerberus
External links
⚠ For reference only. Not for emergency response.