[ Top ] [ Japanese ]
Karasawa Lavas Takahashi and Nishiki, 2006
- Type locality: Karasawa creek, Saku city, Nagano prefecture
- Volcanic rocks
- early Pleistocene (1.00 - 0.98 Ma, K-Ar)
- Lithofacies: Basalt
- Lithofacies: Lavas (more than 10 flow units), Debris flow deposits
- Source: Tokin-no-iwa rock - Okawara pass
- Eruptive volume: 6.7 km3
- Thickness (Overall): 30 - 350 m
- Thickness (A unit): 1 - 5 m
- Lower limit: Nagato Lavas
------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown
- Distribution: 1,500 - 2,000 m above sea level, Karasawa creek - Kakuma river, Saku city, Nagano pref.; 1,100 - 1,450 m above sea level, Manita creek, Saku city, Nagano pref.
- Nishiki and Takahashi (2012) Jour. Geol. Soc. Japan, vol.118, no.8, pp.499-515 DOI