Blödite
Appearance
Blödite | |
---|---|
General | |
Category | Sulfate minerals |
Formula (repeating unit) | Na2Mg(SO4)2·4H2O |
Strunz classification | 7.CC.50 |
Crystal system | Monoclinic |
Crystal class | Prismatic (2/m) (same H-M symbol) |
Space group | P21/a |
Unit cell | a = 11.04 Å, b = 8.15 Å, c = 5.49 Å; β = 100.41°; Z = 2 |
Identification | |
Color | Colorless, yellow, may be dark gray, bluish green, or reddish due to inclusions |
Crystal habit | Prismatic to equant crystals, granular, massive |
Fracture | Conchoidal |
Tenacity | Brittle |
Mohs scale hardness | 2.5 - 3 |
Luster | Vitreous |
Specific gravity | 2.23 |
Optical properties | Biaxial (-) |
Refractive index | nα = 1.483, nβ = 1.486, nγ = 1.487 |
Birefringence | δ = 0.004 |
2V angle | 71° (measured) |
References | [1][2][3] |
Blödite or bloedite is a hydrated sodium magnesium sulfate mineral with formula: Na2Mg(SO4)2·4H2O. The mineral is clear to yellow in color often darkened by inclusions and forms monoclinic crystals.
Blödite was first described in 1821 for an occurrence in a salt deposit in Ischler Salzberg, Bad Ischl, Gmunden, Austria and named for German mineralogist and chemist Karl August Blöde (1773–1820).[2][3]
It is found worldwide in evaporitic sedimentary environments such as the Great Salt Lake, Utah.
See also
References
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