[ Top ] [ Japanese ]
Kumagatake Upper Lava and Pyroclastic Rock Ishige and Nakagawa, 2017
Abbr. KU
- Type locality: 2,140 m above sea level, Crater, Mount Kumagatake, Mount Taisetsu, Hokkaido
- Volcanic rocks
- Pleistocene
- Lithofacies: Lava, Welded pyroclastic fall deposit composed of scoria
- Lithofacies (Main): Hornblende-bearing clinopyroxene-orthopyroxene dacite
- Lithofacies (Minor): Clinopyroxene-orthopyroxene andesite
- Source: Kumagatake summit No.2 crater
- Eruptive volume: < 0.05 km3 DRE
- Thickness (Lava): 50 m
- Thickness (Pyroclastic rocks): 5 m
- Upper limit: Unconformity
- Lower limit: Unconformity
------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown
- Distribution: Northwest of Mount Kumagatake, Mount Taisetsu, Hokkaido
- Ishige and Nakagawa (2017) Jour. Geol. Soc. Japan, vol.123, no.2, pp.73-91, DOI