Daikoku Lava

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Daikoku Lava

Volcanic rocks
Pleistocene

Lithofacies: Biotite olivine quartz-bearing augite hypersthene hornblende andesite lava

Source: in the vicinity of Mount Daikokudake
Thickness: ca. 70 m
Lower limit: Unconformity (Kikyogahara Lava, Fujimi Lava)

Eboshi volcano
[ Upper ]
~~~~~~~~~~~~~~
Marishiten Lava
~~~~~~~~~~~~~~
Daikoku Lava
~~~~~~~~~~~~~~
Kikyogahara Lava
~~~~~~~~~~~~~~
Fujimi Lava
~~~~~~~~~~~~~~
Maekawa Lava
~~~~~~~~~~~~~~
Eboshi Lava
~~~~~~~~~~~~~~
[ Lower ]

Older stage
[ Upper ]
~~~~~~~~~~~~~~
Takamagahara volcano
~~~~~~~~~~~~~~
Eboshi volcano
~~~~~~~~~~~~~~
Sencho volcano
~~~~~~~~~~~~~~
[ Lower ]

Norikura volcano
[ Younger ]
~~~~~~~~~~~~~~
Later stage
~~~~~~~~~~~~~~
Older stage
~~~~~~~~~~~~~~
[ Older ]

------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown

Distribution: Mount Daikokudake, Takayama city, Gifu pref. - Matsumoto city, Nagano pref.

Nakano et al. (1995) Geology of the Norikuradake District, Quadrangle Series, Scale 1:50,000, Geological Survey of Japan, 139p. (in Japanese with English abstract 4p.)