Fluorite
Hirukawa, Nakatsugawa city, Gifu pref., Japan
Field of view: 10 mm. Purple fluorite associated with quartz. The purple grains are fluorite, and the surrounding transparent host is gangue quartz.
Recovered from a quartz vein of a pneumatolytic deposit formed near the boundary between welded tuff and S-type (Ilmenite-series) granite, members of a caldera complex. Formed in the Late Cretaceous (70 Ma).
Fluorite from this location was described in 1938.
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)