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Onoharajima volcano

Lava dome 114 m / 374 ft
Japan, 34.05°N / 139.39°E
Current status: (probably) extinct (0 out of 5) | Reports
Onoharajima volcano books
Typical eruption style: unspecified
Onoharajima volcano eruptions: None during the past 10,000 years
Less than few million years ago (Pleistocene) No recent earthquakes
TimeMag. / DepthDistanceLocation

Background:

Onoharajima is considered to be situated behind the true front of the Izu Volcanic Arc, along a line of volcanoes that is oblique to the Izu Trench. The volcanic rocks of this lineament are characterized by high-alumina basalts, calc-alkaline basalts, andesites, and rhyolites (Onuma et al., 1983). Onoharajima is dominated by andesites of calc-alkaline composition (Onuma et al., 1983).
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Source: Smithsonian / GVP volcano information


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