Rusia · Kaldera
Ushishir
Ushishur
- Tipe
- Kaldera
- Ketinggian
- 357 m
- Letusan terakhir
- 1884

- Tipe
- Kaldera
- Negara
- Rusia
- Wilayah
- Pasifik Barat Laut / Kuril Volcanic Arc
- Ketinggian
- 357 m
- Koordinat
- 47.513, 152.814
- Letusan terakhir
- 1884
- Kondisi tektonik
- Zona subduksi / Kerak samudra (< 15 km)
- Bentuk lahan
- Kaldera
- Batuan utama
- Andesit / Andesit basaltik
Ringkasan geologi
The subaerial portion of Ushishur volcano in the central Kuriles is exposed in two small islands, the southern containing the summit caldera and the northern a portion of the volcano's flanks. A small 1.6-km-wide caldera that formed about 9,400 years ago is narrowly breached on the south, allowing seawater to fill the caldera. Two andesitic lava domes occupy part of the caldera bay; two other older domes are joined by a sand bar to the SE caldera wall. The two younger domes, erupted sometime after the 1769 visit of Captain Snow, form islands in the bay. A cluster of strong fumaroles and hot springs are present along the SE caldera shoreline, and vigorous submarine hydrothermal activity has modified the geochemistry of water within the caldera bay. Aside from growth of the two younger lava domes, only minor phreatic eruptions have been recorded.
Ringkasan Wikipedia
Ringkasan InggrisUshishir is a collective name for two uninhabited volcanic islands and several reefs, all being parts of an eponymous partially submerged volcano, 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 "hot spring".
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Riwayat letusan
4 tercatatGlosariumGaris waktu rinci
- 1884VEI 1Teramati1884-07-16 – akhir tidak diketahuiSE caldera wall
- 1769VEI ?Teramati1769 – akhir tidak diketahuiCenter of caldera bay
- 1710 (±10 tahun)VEI 1Teramati1710 – akhir tidak diketahuiSE caldera wall
- 7450 SM (±50 tahun)VEI 4Perkiraan geologi7450 SM – akhir tidak diketahui
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