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M1
- Accretionary complex
- middle - late Eocene
- Sedimentary facies: Marine
- Lithofacies: Sandstone, Sandstone-dominant interbedded sandstone and mudstone
- Sedimentary structures: Parallel stratification, Cross stratification, Flute marks, Groove marks, Slump structure
- Paleocurrent: from East-northeast
- Thickness: ca. 500 - 1,100 m
- Lower limit: Conformity (W2)
------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown
- Distribution: Hisohara - Kobushigawa river, Kozagawa city, Higashimuro county, Wakayama pref.; Ogama - Esumigawa river - Harihakotoge pass - Kotonotoge pass - Susami - Ichihara - Sumikidani valley - Wabukagawa river - Nishikurigaito - Okanokuroshima island - Cape Esuzaki - Nagai - Unohirami - Sanzaki, Susami city, Nishimuro county, Wakayama pref.
- Fossils (Trace fossils): Paleodictyon isp.
- Tokuoka et al (1981) Geology of the Ryujin District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, 69p. (in Japanese with English abstract 6p.)
- Tateishi et al. (1979) Geology of the Esumi District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, 65p. (in Japanese with English abstract 6p.)