Krenitsyn Volcano
Tao-Rusyr Caldera
Stratovolcano · Russia · 1272m

- Type
- Stratovolcano
- Country
- Russia
- Region
- Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
- Elevation
- 1272m
- Coordinates
- 49.340, 154.725
- Last eruption
- 1952
- Tectonic setting
- Subduction zone / Intermediate crust (15-25 km)
- Landform
- Composite
- Major rock type
- Andesite / Basaltic Andesite
Geological summary
The southern half of Onekotan Island in the northern Kuril Islands contains the 7.5-km-wide Tao-Rusyr caldera, which is mostly filled by Kal'tsevoe lake. The basaltic-to-andesitic caldera formed about 7,500 years ago, in which the large post-caldera Krenitsyn Peak grew, building a 4-km-wide island in the NW part of the lake that rises above the caldera rim. A 350-m-wide, 100-m-deep crater truncates the peak, and a large crater is located on the upper NE side. An eruption in 1952 formed a small lava dome in an explosion crater along the eastern shore of the island.
Eruption history
Summary (VEI over time)
Click a bar to see individual eruptions
Detailed timeline
- 1952VEI 3Observed1952-11-12 – 1952-11-19Krenitsyn Peak (east flank)
- 5550 BCE (±75 yrs)VEI 6Geological estimateBCE 5550 – OngoingTao-Rusyr
External links
- Not yet on Wikipedia (English). You can contribute on Wikidata.
- 🔗 Smithsonian GVP source page
⚠ For reference only. Not for emergency response.