Appidakechienosawa Lava

[ Top ] [ Japanese ]

Appidakechienosawa Lava

Type locality: Mount Appidake, Hachimantai city, Iwate prefecture
Volcanic rocks
Pleistocene - Holocene

Lithofacies: Olivine augite hypersthene andesite

Source: triangulation station of Mount Appidake
Running distance: ca. 2 km

Hachimantai volcano
[ Upper ]
~~~~~~~~~~~~~~
Appidakechienosawa Lava
~~~~~~~~~~~~~~
Appidake Lava
~~~~~~~~~~~~~~
Gentamori Lava
~~~~~~~~~~~~~~
Hachimantai Lava
~~~~~~~~~~~~~~
Mokkodake Lava
~~~~~~~~~~~~~~
Hachimantai-Nishikabu Lava
~~~~~~~~~~~~~~
Kuragata Lava
~~~~~~~~~~~~~~
Yudamatagawa Lava
~~~~~~~~~~~~~~
Komonomori Agglomerate
~~~~~~~~~~~~~~
[ Lower ]

Hachimantai volcanic group
[ Upper ]
~~~~~~~~~~~~~~
Obukadake volcano
~~~~~~~~~~~~~~
Chausudake volcano
~~~~~~~~~~~~~~
Hachimantai volcano
~~~~~~~~~~~~~~
[ Lower ]

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

Distribution: Mount Appidake - Chienosawa creek, Hachimantai city, Iwate pref.

Kawano and Uemura (1964) Hachimantai, Explanatory Text of the Geological Map of Japan, Scale 1:50,000, Geological Survey of Japan, 36p. (in Japanese with English abstract 8p.)