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Fudokabe Andesite

• Coherent formation
• early - late Miocene
• Intruded in: Zasunbo Alternation of Conglomerate, Sandstone and Mudstone Member, Mekka Pumiceous Tuff Member

• Lithofacies: Hypersthene augite andesite

• Distribution (Diameter): ca. 500 m

• Distribution: Iseya - Fudokabe cliff - Zashubo, Tateyama 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.)