Smirnov
Ruruidake [Smirnov]
Stratovolcano · Japan - administered by Russia · 1447m
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- Type
- Stratovolcano
- Country
- Japan - administered by Russia
- Region
- Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
- Elevation
- 1447m
- Coordinates
- 44.454, 146.140
- Last eruption
- Unknown
- Tectonic setting
- Subduction zone / Intermediate crust (15-25 km)
- Landform
- Composite
- Major rock type
- Andesite / Basaltic Andesite
Geological summary
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.
From Wikipedia
Smirnov 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.
Wikipedia · CC BY-SA · Read full article →
Eruption history
Detailed timeline
No eruption records available.
External links
⚠ For reference only. Not for emergency response.