Rusia · Kerucut piroklastik
Tolmachev Dol
- Tipe
- Kerucut piroklastik
- Ketinggian
- 1021 m
- Letusan terakhir
- 300

- Tipe
- Kerucut piroklastik
- Negara
- Rusia
- Wilayah
- Pasifik Barat Laut / Kuril Volcanic Arc
- Ketinggian
- 1021 m
- Koordinat
- 52.630, 157.580
- Letusan terakhir
- 300
- Kondisi tektonik
- Zona subduksi / Kerak benua (> 25 km)
- Bentuk lahan
- Gugusan gunung api
- Batuan utama
- Basal / Pikrobasal
Ringkasan geologi
Tolmachev Dol (Tomachev Plateau) is broad volcanic highland NE of Opala volcano that includes numerous late-Pleistocene and Holocene cinder cones and associated lava flows. The cones and lava fields cover a broad area on both sides of Lake Tolmachev, which lies in large depression halfway between Opala and Gorely volcanoes. The Pleistocene Tolmachev stratovolcano lies on the SE side of the lake. A major explosive eruption took place about 4,600 years ago from Chasha crater in the northern part of the plateau, during which about 1 km3 of rhyolitic tephra was ejected. The latest dated eruption occurred from a cinder cone in the NW part of the plateau about 1,600-1,700 years ago.
Riwayat letusan
2 tercatatGlosariumGaris waktu rinci
- 300 (±150 tahun)VEI ?Perkiraan geologi300 – akhir tidak diketahuiNW part of Tolmachev Dol
- 2650 SMVEI 4Perkiraan geologi2650 SM – akhir tidak diketahuiChasha crater
Gunung api terdekat
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.