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Fudeshima volcano
- Volcanic rocks
- Stratovolcano
- late Pliocene - Pleistocene (< 2.41 Ma, K-Ar)
- Intruded by: Basalt dikes
- Lithofacies: Low-alkaline tholeiite series
- Lithofacies: Pyroxene olivine basalt, Olivine basalt lava, Scoria fall deposit, Welded spatter, Vent-fill breccia
- Source: in the vicinity of Fudeshima island
- Thickness: 950 m
- Distribution: 3.5 km or more
- Upper limit: Unconformity (Older edifice)
- Distribution: southern part of east coast of Izu-Oshima island
- Distribution: opposite bank of Fudeshima island - Funo fall - Kakihara shore - Nejinohana, Oshima city, Tokyo
- Isshiki (1984) Geology of the Oshima District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, 133p. (in Japanese with English abstract 5p.)