Tolmachev Dol
Kerucut piroklastik · Russia · 1021 m

- Tipe
- Kerucut piroklastik
- Negara
- Russia
- Wilayah
- Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
- Ketinggian
- 1021 m
- Koordinat
- 52.630, 157.580
- Letusan terakhir
- 300
- Kondisi tektonik
- Subduction zone / Continental crust (> 25 km)
- Bentuk lahan
- Cluster
- Batuan utama
- Basalt / Picro-Basalt
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.
Ringkasan Wikipedia
Ringkasan InggrisTolmachev Dol is a volcanic highland located in the southern part of Kamchatka Peninsula, Russia, northeast of Opala volcano. The cones and lava fields cover a broad area around Tolmachev Lake within the intermountain Tolmachev depression of area about 650 sq.km.
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Riwayat letusan
Garis waktu rinci
- 300 (±150 tahun)VEI ?Perkiraan geologi300 – BerlangsungNW part of Tolmachev Dol
- 2650 SMVEI 4Perkiraan geologiBCE 2650 – BerlangsungChasha crater
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.