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Mitsudake Lava
- Volcanic rocks
- Pleistocene
- Lithofacies: Hypersthene augite andesite lava
- Paleocurrent: East
- Source: Flank Lake Nanatsuike, a crater of Mount Yokodake
- Running distance: 850, 1,300 m
- Upper limit: Unconformity (Odake Lava)
- Lower limit: Unconformity (Chuokako Lava)
------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown
- Distribution: Mount Mitsudake, Sakuho city, Minamisaku county, Nagano pref.; Tengunoroji, Tateshina city, Kitasaku county, 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.)