Ketoy
Ketoi
Stratovolcano · Russia · 1172m

- Type
- Stratovolcano
- Country
- Russia
- Region
- Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
- Elevation
- 1172m
- Coordinates
- 47.350, 152.475
- Last eruption
- 1960
- Tectonic setting
- Subduction zone / Oceanic crust (< 15 km)
- Landform
- Composite
- Major rock type
- Andesite / Basaltic Andesite
Geological summary
The circular 10-km-wide Ketoi island, which rises across the 19-km-wide Diana Strait from Simushir Island, hosts of one of the most complex volcanic structures of the Kuril Islands. The rim of a 5-km-wide Pleistocene caldera is exposed only on the NE side. A younger stratovolcano forming the NW part of the island is cut by a horst-and-graben structure containing two solfatara fields. A 1.5-km-wide freshwater lake fills an explosion crater in the center of the island. Pallas Peak, a large andesitic cone in the NE part of the caldera, is truncated by a 550-m-wide crater containing a brilliantly colored turquoise crater lake. Lava flows from Pallas Peak overtop the caldera rim and descend nearly 5 km to the SE coast. The first historical eruption of Pallas Peak, during 1843-46, was its largest.
From Wikipedia
Ketoy is an uninhabited volcanic island located in the centre of the Kuril Islands chain in the Sea of Okhotsk in the northwest Pacific Ocean. Its name is derived from the Ainu language for "skeleton" or "bad".
Wikipedia · CC BY-SA · Read full article →
Eruption history
Detailed timeline
- 2018VEI 1Observed2018-09-21 – 2018-09-21
- 2013VEI ?Observed2013-07-25 – 2013-08-12Pallas Peak
- 1960VEI 2Observed1960-09-27 – OngoingPallas Peak
- 1924VEI 2Observed1924 – OngoingPallas Peak
- 1843VEI 2Observed1843-07 – 1846Pallas Peak
External links
⚠ For reference only. Not for emergency response.