rynersonite
Sign in to saveAlso known as IMA1974-058
Rynersonite is an oxide mineral. It crystallizes in the orthorhombic crystal system. It is dull, translucent mineral, fibrous in nature. Usually off-white to pale pink in color. It occurs in granitic pegmatites and was first described for an occurrence in San Diego County, California in 1978.
In the Vinony graph
Within Vinony's link graph, rynersonite is referenced by 4 other articles, and connects out to Uganda, Colorado and Kampala.
It is catalogued under topics including Minerals described in 1978, Minerals in space group 62 and Niobium minerals.
Its subject is documented across 7 Wikipedia language editions.
Wikidata facts
- Image
- Rynersonite.jpg
Show 5 more facts
- Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
- 4.DF.05
- Nickel-Strunz 9th edition (updated 2009)
- 4.DF.05
- chemical formula
- CaTa₂O₆
- IMA Mineral Symbol
- Rys
- Commons category
- Rynersonite
Sources (1)
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Encyclopedic overview
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- References
Rynersonite is an oxide mineral. It crystallizes in the orthorhombic crystal system. It is dull, translucent mineral, fibrous in nature. Usually off-white to pale pink in color. It occurs in granitic pegmatites and was first described for an occurrence in San Diego County, California in 1978.
Besides the San Diego, California area, Rynersonite is also found in Colorado and Kampala, Uganda.
Excerpted from Wikipedia’s “rynersonite” article, available under the CC BY-SA 4.0 licence.