tincalconite
Sign in to saveTincalconite is a hydrous sodium borate mineral closely related to borax, and is a secondary mineral that forms as a dehydration product of borax. Its formula is Na2B4O7·5H2O or Na2[B4O5(OH)4]·3H2O.
In the Vinony graph
Vinony's link graph records 9 inbound references to tincalconite, and connects out to hexagonal crystal system, water and California.
Vinony files it under Minerals described in 1878, Minerals in space group 155 and Nesoborates.
Vinony links it to 9 Wikipedia language editions.
Key facts
- Mineral.name
- Tincalconite
- Mineral.image
- TincalconiteUSGOV.jpg
- Mineral.imagesize
- 260px
- Mineral.category
- Nesoborates
- Mineral.formula
- Na2[B4O5(OH)4]·3H2O
- Mineral.IMAsymbol
- Tnc
- Mineral.strunz
- 6.DA.15
- Mineral.system
- Trigonal
- Mineral.class
- Trapezohedral (32) H-M symbol: (32)
- Mineral.symmetry
- R32
via Wikipedia infobox
Wikidata facts
- Named after
- powder
- Image
- TincalconiteUSGOV.jpg
Show 8 more facts
- Commons category
- Tincalconite
- Nickel-Strunz 9th edition (updated 2009)
- 6.DA.15
- Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
- 6.DA.15
- type locality (geology)
- Searles Lake
- crystal system
- trigonal crystal system
- IMA Mineral Symbol
- Tnc
- chemical formula
- Na₂B₄O₅(OH)₄·3H₂O
- Strunz 8th edition (series ID, updated)
- Vc/B.05
Sources (1)
via Wikidata · CC0
~2 min read
Encyclopedic overview
2 sectionsContents
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- References
Tincalconite is a hydrous sodium borate mineral closely related to borax, and is a secondary mineral that forms as a dehydration product of borax. Its formula is Na2B4O7·5H2O or Na2[B4O5(OH)4]·3H2O.
Tincalconite typically occurs as a fine grained white powder. It crystallizes in the hexagonal crystal system and has been found as primary euhedral di-rhombohedral, pseudo-octahedral crystals. It is also found pseudomorphically replacing borax crystals. It has a specific gravity of 1.88 and a Mohs hardness of 2. Refractive index values are nω=1.460 and nε=1.470.
Excerpted from Wikipedia’s “tincalconite” article, available under the CC BY-SA 4.0 licence.