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Kohisagawa Member Kubo et al., 2002
- Type locality: Kohisa river, Ohisa town, Iwaki city, Fukushima prefecture
- Coherent formation
- southern Yezo Forearc basin (Jobanoki basin)
- Late Cretaceous, late Coniacian
- Sedimentary facies: Fluvial
- Sedimentary facies (Minor): Marine
- Sedimentary facies: Braided river
- Lithofacies: Sandstone
- Lithofacies (Minor): Conglomerate
- Sedimentary structures: Cross stratification, Bioturbation, Tuff
- Thickness: ca. 185 - 240 m
- Upper limit: Bottom of conglomerate bed
- Upper limit: Conformity (Irimazawa Member), Unconformity (Shiramizu Group)
- Lower limit: Bottom of the very thick sandy siltstone-deficient sandstone bed
- Lower limit: Unconformity (Kasamatsu Formation)
------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown
- Distribution: Ohisa - Kohisa river, Ohisa town, Iwaki city, Fukushima pref.; Komatsu, Hirono city, Futaba county, Fukushima pref.
- Fossils: Dinosaurs (Diplodocus sp., Teeth), Insects (in Amber), Pipe rocks
- Fossils (Plants): Esgueiria sp. (Flowers), Pollen, Spores
- Ando et al. (2011) Jour. Geol. Soc. Japan, vol.117, Supplement, pp.49-67 DOI
- Kubo et al. (2002) Geology of the Kawamae and Ide District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, AIST, 136p. (in Japanese with English abstract 6p.)