[ Top ] [ Japanese ]
Ko-a Tephra
Abbr.: Ko-a
- Type locality: Mount Komagatake, Hokkaido
- Tephra
- Holocene (June 17th, 1929)
- Lithofacies: Pumice fall deposit (5 fall units), Pyroclastic flow deposit (more than 2 units), Pyroclastic surge deposit
- Mode of eruption: Plinian associated with pyroclastic flow deposit
- Eruptive volume (Pumice): ca. 0.38 km3
- Eruptive volume (Pyroclastic flow): ca. 0.14 km3
- Thickness (Erupted): 106 - 154 cm
- Thickness (Present): 70 - 120 cm
- Ko-a
- [ Upper ]
- ~~~~~~~~~~~~~~
- Ko-a1
- ~~~~~~~~~~~~~~
- Ko-a2
- ~~~~~~~~~~~~~~
- Ko-a3
- ~~~~~~~~~~~~~~
- Ko-a4
- ~~~~~~~~~~~~~~
- Ko-a5
- ~~~~~~~~~~~~~~
- [ Lower ]
------ Conformity, ~~~~~~ Unconformity, ~~~--- Local unconformity, '''/,, Interfingered, :::::: Fault, /--/-- Thrust, +__+__ Ground surface, ?--?-- Unknown
- Distribution: Mount Komagatake, Hokkaido
- Distribution: Cape Dekima, Shikabe city, Kayabe county, Hokkaido
- Yoshimoto et al. (2008) Jour. Geol. Soc. Japan, vol.114, no.7, pp.336-347 DOI
- Yoshimoto et al. (2007) Jour. Geol. Soc. Japan, vol.113, Supplement, pp.81-92 DOI