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Dedana Formation (Otsuka, 1932) Takano, 1994
- Type locality: Yomiuri Golf Club, Yanokuchi, Inagi city, Tokyo
- Coherent formation
- Fore-arc basin sediments (Kazusa trough)
- early Pleistocene (1.5 - 1.3 Ma)
- Interfingered: Ozenji Formation
- Interfingered (Lower): Kakio Formation
- Lithofacies: Sands
- Lithofacies (Middle): Mud
- Lithofacies (Middle, Minor): Wood fragments
- Lithofacies (Minor): Gravels
- Sedimentary structures: Cross stratification, Parallel stratification
- Thickness: 15 - 125 m
- Thickness (Middle): 5 m or thicker
- Thickness (Lower): 3 - 10 m
- Upper limit: Conformity (Ikuta Formation), Unconformity (Gotentoge Terrace Deposit)
- Lower limit: Top of the horizon intercalating many conglomerate beds
- Lower limit: Conformity (Inagi Formation)
------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown
- Distribution: Yanokuchi - Wakabadai - Koyodai - Sakahama, Inagi city, Tokyo; Suge, Tama ward, Kawasaki city, Kanagawa pref.; Hosoyama - Chiyogaoka - Takaishi - Yurigaoka, Asao ward, Kawasaki city, Kanagawa pref.
- Tephra: Hosoyama Tuff, MT
- Suzuki et al. (2016) Jour. Geol. Soc. Japan, vol.122, no.7, pp.343-356, DOI
- Ueki et al. (2013) Geology of the Hachioji District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, AIST, 137p. (in Japanese with English abstract 6p.)
- Suzuki and Murata (2011) Jour. Geol. Soc. Japan, vol.117, no.7, pp.379-397 DOI
- Oka et al. (1984) Geology of the Tokyo-Seinambu District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, 148p. (in Japanese with English abstract 7p.)