hydrokenoelsmoreite
Sign in to saveAlso known as elsmoreite, IMA2003-059
Hydrokenoelsmoreite is a hydrous tungsten oxide mineral with formula □2W2O6(H2O). Hydrokenoelsmoreite is a colorless to white, translucent isometric mineral. It has a Mohs hardness of 3, exhibits no cleavage and has a splintery fracture. It has a vitreous to adamantine luster. It is optically isotropic with an index of refraction of n = 2.24.
In the Vinony graph
Within Vinony's link graph, hydrokenoelsmoreite is referenced by 16 other articles, and connects out to Mohs scale of mineral hardness, cubic crystal system and oxide class of minerals.
Vinony files it under Cubic minerals, Minerals in space group 227 and Oxide minerals.
Its subject is documented across 5 Wikipedia language editions.
Wikidata facts
- Named after
- vacancy
- Image
- Hydrokenoelsmoreite-Stolzite-418719.jpg
Show 6 more facts
- streak color
- white
- Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
- 4.DH.15
- type locality (geology)
- Stevens County
- Commons category
- Hydrokenoelsmoreite
- IMA Mineral Symbol
- Hkm
- chemical formula
- ☐₂W₂O₆(H₂O)
via Wikidata · CC0
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Encyclopedic overview
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- References
Hydrokenoelsmoreite is a hydrous tungsten oxide mineral with formula □2W2O6(H2O). Hydrokenoelsmoreite is a colorless to white, translucent isometric mineral. It has a Mohs hardness of 3, exhibits no cleavage and has a splintery fracture. It has a vitreous to adamantine luster. It is optically isotropic with an index of refraction of n = 2.24.
It forms from the oxidation of ferberite within granitic pegmatite dykes and in pegmatitic greisen veins. It has a structure based on a defect pyrochlore lattice (A2B2O6O’).
Excerpted from Wikipedia’s “hydrokenoelsmoreite” article, available under the CC BY-SA 4.0 licence.