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Tomogasihma Formation Ishigami and Yoshimatsu, 1972
- Type locality: Tomogashima island, Wakayama city, Wakayama prefecture
- Coherent formation
- Izumi sedimentary basin
- Forearc basin associated with strike-slip fault related to Median Tectonic Line
- Late Cretaceous, Maastrichtian
- Sedimentary facies: Main filling of the sedimentary basin
- Lithofacies: Turbidite, Channel deposit
- Lithofacies: Interbedded sandstone and mudstone, Interbedded conglomerate and sandstone
- Lithofacies (Minor): Felsic tuff
- Sedimentary structures: Flute marks, Groove marks, Load structure, Current ripples, Slump structures
- Paleocurrent: from Northeast to Southwest
- Thickness: ca. 720 - 780 m
------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown
- Distribution: Okinoshima island - Chinoshima island, Wakayama city, Wakayama pref.
- Fossils: Ammonoids (Baculites regina), Shellfishes (Acila sp., Portlandia izumensis, Nanovavis sp.), Achaeozostera sp.
- Miyata et al. (1993) Geology of the Wakayama and Ozaki District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, 68p. (in Japanese with English abstract 4p.)