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Osawa Conglomerate

• Coherent formation
• Paleogene

• Sedimentary facies: Fluvial?
• Lithofacies: Conglomerate

• Thickness: ca. 10 m
• Lower limit: Unconformity (Kogigawa Granite)

• Distribution: Ushitakigawa river, Osawa town, Kishiwada city, Osaka pref.

• Itihara et al. (1986) Geology of the Kishiwada District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, 148p. (in Japanese with English abstract 7p.)