nyerereite
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Nyerereite is a very rare sodium calcium carbonate mineral with formula Na2Ca(CO3)2. It forms colorless, platey pseudohexagonal orthorhombic crystals that are typically twinned. It has a specific gravity of 2.54 and indices of refraction of nα=1.511, nβ=1.533 and nγ=1.535. Nyerereite is not stable in contact with the atmosphere and rapidly breaks down. Collection specimens must be kept in a sealed argon environment.
Wikidata facts
- Subclass of
- carbonate and nitrate class of minerals
- Named after
- Julius Nyerere
- Image
- Nyerereite.jpg
Show 9 more facts
- Nickel-Strunz 9th edition (updated 2009)
- 5.AC.10
- Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
- 5.AC.10
- type locality (geology)
- Ol Doinyo Lengai
- streak color
- white
- crystal system
- orthorhombic crystal system
- Commons category
- Nyerereite
- IMA Mineral Symbol
- Nye
- chemical formula
- Na₂Ca(CO₃)₂
- Strunz 8th edition (series ID, updated)
- Vb/A.05
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Encyclopedic overview
4 sectionsContents
- Special characteristics
- Occurrence and discovery
- References
- Bibliography
Nyerereite is a very rare sodium calcium carbonate mineral with formula Na2Ca(CO3)2. It forms colorless, platey pseudohexagonal orthorhombic crystals that are typically twinned. It has a specific gravity of 2.54 and indices of refraction of nα=1.511, nβ=1.533 and nγ=1.535. Nyerereite is not stable in contact with the atmosphere and rapidly breaks down. Collection specimens must be kept in a sealed argon environment.
It has a Hermann–Mauguin notation of mm2 and the respective space group is Cmc21. In nature Nyerereite is naturally twinned and is pseudohexagonal with triad twinning; meaning that this is a six sided crystal that apparently has a hexagonal shape but is not in the hexagonal system. Triad twinning is the intergrowth of three orthorhombic crystals that turn at their center and form hexagonally shaped crystals. Nyerereite is biaxial negative, and has a 2v of 29 degrees. It shows a center acute bisectrix and a birefringence of approximately 0.023. At high temperatures or just erupted lava nyerereite is uniaxial and shows an interference color of second order blue when twinning is not present, and when twinning is there the interference color of nyerereite is first order grey.
Excerpted from Wikipedia’s “nyerereite” article, available under the CC BY-SA 4.0 licence.