Smirnov
Ruruidake [Smirnov]
Stratovolkan · Japan - administered by Russia · 1447 m
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- Tipe
- Stratovolkan
- Negara
- Japan - administered by Russia
- Wilayah
- Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
- Ketinggian
- 1447 m
- Koordinat
- 44.454, 146.140
- Letusan terakhir
- Tidak diketahui
- Kondisi tektonik
- Subduction zone / Intermediate crust (15-25 km)
- Bentuk lahan
- Composite
- Batuan utama
- Andesite / Basaltic Andesite
Ringkasan geologi
Ruruidake is a late-Pleistocene andesitic-to-dacitic volcanic complex on the NW tip of Kunashir Island in the southern Kuriles, NW of Chachadake [Tiatia} volcano. About 2.5 km SSW of the Ruruidake peak, the gently sloping Smirnov edifice partially retains a constructional form, but the southern side has been heavily eroded by glaciers, exposing its Tertiary basement. A wide glacial trough on the SE flank of Smirnov contains a pyroclastic cone at its head that fed a 4 km lava flow. Another pyroclastic cone is located at the base of the trough near the terminus of the lava flow. Two fresh-looking lava domes of Holocene age also lie within the glacial valley to the north.
Ringkasan Wikipedia
Ringkasan InggrisSmirnov is a volcano located at the northwestern end of Kunashir Island, Kuril Islands, Russia. It consists of two summits: Smirnov and Rurui stratovolcanoes. Rurui is the higher summit.
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