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N1 Member
- Type locality: Oshima city, Tokyo
- Volcanic rocks
- Stratovolcano, Caldera volcano
- Holocene (12th century)
- Sedimentary facies (Lower): Scoria cones (2 cones)
- Lithofacies: Low-alkaline tholeiite series
- Lithofacies: Pigeonite series
- Lithofacies (Upper): Volcanic ash
- Lithofacies (Upper, Minor): Accretionary lapilli tuff
- Lithofacies (Lower): Interbedded scoria fall deposit and lapilli tuff, Lava (2 flow units)
- Lithofacies (Lower, Minor): Reworked scoria
- Thickness (Upper): 12 cm
- Thickness (Lower): 730 cm or thicker
- Running distance (Eastern lava): 0.9 km
- Running distance (Western lava): 1.3 km
- Upper limit: Unconformity (Y6 Member)
------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown
- Distribution: 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.)