ruizite
Sign in to saveAlso known as IMA1977-007
Ruizite is a sorosilicate mineral with formula Ca2Mn2Si4O11(OH)4·2H2O. It was discovered at the Christmas mine in Christmas, Arizona, and described in 1977. The mineral is named for discoverer Joe Ana Ruiz.
Wikidata facts
- Image
- Ruizite-Calcite-180789.jpg
Show 5 more facts
- Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
- 9.BJ.35
- Nickel-Strunz 9th edition (updated 2009)
- 9.BJ.35
- Commons category
- Ruizite
- IMA Mineral Symbol
- Rz
- chemical formula
- Ca₂Mn³⁺₂[Si₄O₁₁(OH)₂](OH)₂*₂H₂O
Sources (2)
via Wikidata · CC0
~4 min read
Article
7 sectionsContents
- Description and occurrence
- Crystal structure and chemistry
- History
- See also
- References
- Further reading
- External links
{{Infobox mineral | name = Ruizite | category = Sorosilicate | boxwidth = | boxbgcolor = | image = Ruizite-Calcite-180789.jpg | imagesize = 260px | caption = Clusters of ruizite on calcite from South Africa | formula = Ca2Mn2Si4O11(OH)4·2H2O | IMAsymbol = Rz | molweight = | strunz = 9.BJ.35 | dana = 57.2.2.1 | system = Monoclinic | class = Prismatic (2/m) (same H-M symbol) | symmetry = P21/c | unit cell = a = 11.95 Å, b = 6.17 Å c = 9.03 Å, β = 91.37°; Z = 4 | color = Orange, red-brown | habit = | twinning = Common on {100} | cleavage = | fracture = | tenacity = | mohs = 5 | luster = | polish = | refractive = nα = 1.663nβ = 1.715nγ = 1.734 | opticalprop = Biaxial (-) | birefringence = δ = 0.071 | 2V = 60° | dispersion = | pleochroism = | fluorescence= | absorption = | streak = Apricot | gravity = | density = | melt = | fusibility = | diagnostic = | solubility = | diaphaneity = Translucent | other = | references = }} Ruizite is a sorosilicate mineral with formula Ca2Mn2Si4O11(OH)4·2H2O. It was discovered at the Christmas mine in Christmas, Arizona, and described in 1977. The mineral is named for discoverer Joe Ana Ruiz.
==Description and occurrence== thumb|left|Ruizite from Arizona Ruizite is translucent and orange to red-brown in color with an apricot yellow streak. The mineral occurs as euhedral prisms up to or as radial clusters of acicular (needle-like) crystals.