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

- Tipe
- Stratovolkan
- Negara
- Russia
- Wilayah
- Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
- Ketinggian
- 1272 m
- Koordinat
- 49.340, 154.725
- Letusan terakhir
- 1952
- Kondisi tektonik
- Subduction zone / Intermediate crust (15-25 km)
- Bentuk lahan
- Composite
- Batuan utama
- Andesite / Basaltic Andesite
Ringkasan geologi
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.
Riwayat letusan
Ringkasan (VEI dari waktu ke waktu)
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Garis waktu rinci
- 1952VEI 3Teramati1952-11-12 – 1952-11-19Krenitsyn Peak (east flank)
- 5550 SM (±75 tahun)VEI 6Perkiraan geologiBCE 5550 – BerlangsungTao-Rusyr
Tautan eksternal
- Belum ada di Wikipedia (Bahasa Indonesia). Anda dapat berkontribusi di Wikidata.
- 🔗 Halaman asli Smithsonian GVP
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