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Kutsushitajo Lava
- Volcanic rocks
- Pleistocene
- Lithofacies: Hornblende augite hypersthene andesite lava
- Paleocurrent: West
- Source: Flank crater of Mount Yokodake
- Thickness: ca. 50 m
- Distribution (Width): 160 m
- Running distance: 2,200 m
- Lower limit: Unconformity (Chuokako Lava, Yokodake Basal Lava)
------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown
- Distribution: Mount Yokodake, Chino city, Nagano pref.
- Kawachi (1974) Geology of the Tateshinayama District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, 114p. (in Japanese with English abstract 5p.)