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Haruna-Futatsudake-Shibukawa Fall Tephra Geshi and Takeuchi, 2012
- Type locality: Kurosawa river, Ono, Shibukawa city, Gunma prefecture
- Type locality: Takizawa river, Uenohara, Yoshioka city, Kitagunma county, Gunma prefecture
- Tephra
- Holocene (end of 5th century; 489 cal AD, Wiggle matching)
- Sedimentary facies: Pyroclastic fall deposit, Pyroclastic surge
- Lithofacies: Volcanic ash
- Lithofacies (Minor): Accretionry lapilli
- Source: Haruna volcano
- Mode of eruption: Phreatomagmatic
- Thickness: ca. 40 cm - 1.2 m
- Volume: ca. 0.3 km3
------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown
- Distribution: Kurosawa river, Ono, Shibukawa city, Gunma pref.; Takizawa river, Uenohara, Yoshioka city, Kitagunma county, Gunma pref.; Nakano, Misato town, Takasaki city, Gunma pref.
- Geshi and Takeuchi (2012) Geology of the Haruna San District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, AIST, 79p. (in Japanese with English abstract 3p.)