Galena
Iwahana shaft, Hikida Mine
Hikida, Kanuma city, Tochigi pref., Japan
Source for Lead
Field of view: 50 mm. Galena associated with sphalerite and kaolinite. The granular dark gray grains with perfect cleavage are galena, and surrounding massive black parts are sphalerite. The white to gray basement with a vitreous luster is gangue quartz, and the opaque white parts are earthy kaolinite. The brown parts are dirt by limonite.
Recovered from a quartz vein of a moderate-temperature hydrothermal deposit probably associated with welded tuff. Formed in the early Paleocene (65 Ma).
Galena from this location was described in 2008.
Other localities
- Kamioka Mine (Pneumatolytic Skarn, Bedded)
- Chichibu Mine (Hydrothermal Skarn, Granular)
- Kisan-mori Mine (Hydrothermal, Bedded)
- Mikawa Mine (Hydrothermal, Massive)
- Sayama Mine (Hydrothermal, Massive)
- Suzukura Mine (Hydrothermal, Massive)
- Yunosawa Mine (Hydrothermal, Granular)
- Hikida Mine (Hydrothermal, Granular)
- Takanosu Mine (Mn Skarn, Granular)