[ Top ] [ Japanese ]
N3 Member
- Type locality: Oshima city, Tokyo
- Volcanic rocks
- Phreatomagmatic eruption forming Habu port
- Stratovolcano, Caldera volcano
- Holocene (9th century, 1,130 yBP, 14C)
- Lithofacies: Low-alkaline tholeiite series
- Lithofacies: Pigeonite series
- Lithofacies (Upper): Volcanic ash
- Lithofacies (Lower): Scoria fall deposit
- Mode of eruption (Upper): Fissure, Phreatomagmatic
- Mode of eruption (Lower): Strombolian
- Eruptive volume (Upper): 0.05 km3 DRE
- Eruptive volume (Lower): 0.03 km3 DRE
- Thickness: 10 cm - 1 m or thicker
------ 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.)