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Takamineyama volcano

• Coherent formation
• Pleistocene

• Lithofacies: Augite hypersthene andesite tuff breccia
• Lithofacies (Minor): Augite hypersthene andesite lava

• Thickness: ca. 300 m
• Distribution: ca. 24 km²
• Lower limit: Unconformity (Zasunbo Alternation of Conglomerate, Sandstone and Mudstone Member)

• Distribution: Mount Takamineyama - Komatagawa river - Shiraiwagawa river, Kamiichi city, Nakaniikawa county, Toyama pref.

• Nozawa and Sakamoto (1960) Gohyakkoku, Explanatory Text of the Geological Map of Japan, Scale 1:50,000, Geological Survey of Japan, 68p. (in Japanese with English abstract 10p.)