Vilyuchik
Vilyuchinsky
Stratovolkan · Russia · 2173 m

- Tipe
- Stratovolkan
- Negara
- Russia
- Wilayah
- Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
- Ketinggian
- 2173 m
- Koordinat
- 52.700, 158.280
- Letusan terakhir
- -8050
- Kondisi tektonik
- Subduction zone / Continental crust (> 25 km)
- Bentuk lahan
- Composite
- Batuan utama
- Andesite / Basaltic Andesite
Ringkasan geologi
Vilyuchinsky, or Vilyuchik, is a steep-sided Pleistocene-to-Holocene stratovolcano south of Avachinsky Bay. Deep erosional gullies dissect the flanks, with Lava domes and young basaltic cinder cones at its base. Most of the growth of the volcano took place during the late Pleistocene. The last significant eruption took place from the summit crater about 10,000 years ago, producing a moderate airfall deposit and a lava flow. Landslides and rock avalanches have affected habited areas.
Ringkasan Wikipedia
Ringkasan InggrisVilyuchik, also known as Vilyuchinsky is a dormant stratovolcano in the southern part of the Kamchatka Peninsula, Russia. It is located about 30 kilometres (19 mi) SSW of the closed city of Vilyuchinsk.
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Riwayat letusan
Garis waktu rinci
- 8050 SMVEI 2Perkiraan geologiBCE 8050 – Berlangsung
Tautan eksternal
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