Fluorite
Higashi-Mozumi, Kamioka village, Hida city, Gifu pref., Japan
This locality is closed to collecting.
Field of view: 20 mm. Transparent fluorite. The transparent cubes are fluorite. The brown basement is gangue quartz encrusted with limonite.
Recovered from an open space of a quartz vein in a pneumatolytic deposit combined with skarn formed by contact metamorphism of I-type (magnetite-series) granite. Formed in the early Paleocene (65 Ma).
Fluorite from this location was described in 1947.
Other localities
- Hirukawa (Pegmatite, Octahedral)
- Hiraiwa Mine (Hydrothermal, Dodecahedral)
- Goka Mine (Hydrothermal, Massive)
- Takatori Mine (Pneumatolytic, Massive)
- Takane Mine (Pneumatolytic, Massive)
- Kamioka Mine (Pneumatolytic Skarn, Cubic)