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Shuchi Formation Ishida, 1983

• Type locality: Kyoto Tamba Park, Kyotanba city, Funai county, Kyoto prefecture
• Coherent formation
• Miocene - Pliocene

• Lithofacies (Top): Mudstone
• Lithofacies: Conglomerate
• Lithofacies (Minor): Sandstone

• Thickness (Top): ca. 2 m
• Thickness: ca. 25 - 40 m
• Upper limit: Abut unconformity (Ueno Formation), Unconformity (Higher Terrace Deposits)
• Lower limit: Unconformity (Tamba Belt)

• Distribution: Kyoto Tamba Park - Shuchi - Toyota, Kyotanba city, Funai conty, Kyoto pref.

• Imoto et al. (1991) Geology of the Sonobe District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, 68p. (in Japanese with English abstract 4p.)
• Kimura et al. (1989) Geology of the Ayabe District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, 104p. (in Japanese with English abstract 5p.)