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Higashihigasa Formation Otsuka and Mochizuki, 1932
- Type locality: Seri, Futtsu city, Chiba prefecture
- Coherent formation
- Fore-arc basin sediments (Kazusa trough)
- Fan valley-fill deposit at the upper part of submarine fan in Higashihigasa submarine
- Pleistocene
- Correlation (Upper): upper Umegase Formation
- Correlation (Lower): lower Umegase Formation
- Sedimentary facies: Submarine valley opened to east
- Lithofacies: Turbidite
- Lithofacies: Sandstone
- Sedimentary structures: Slump structures, Graded bedding
- Thickness: 200 m
- Distribution (East - West): ca. 10 km
- Distribution (South - North): ca. 1 km
------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown
- Distribution: Seri - Yokoyama - Yamawaki - Higashiowada, Futtsu city, Chiba pref.; Uehata - Higashihigasa, Kimitsu city, Chiba pref.
- Fossils: Mammalia (Parelephas prozimus), Shellfishes
- Nakajima and Watanabe (2005) Geology of the Futtsu District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, AIST, 102p. (in Japanese with English abstract 8p.)