Hisingerite

Hisingerite
Crystallized plates of reddish-brown, silver metallic-lustre hisingerite crystals
General
CategorySilicate mineral
Formula
(repeating unit)
FeIII2Si2O5(OH)4 · 2 H2O
IMA symbolHsg
Strunz classification9.ED.10
Crystal systemMonoclinic
Unknown space group
Unit cella = 5.4, b = 9.03
c = 14.99 [Å]; β = 98.32°; Z = 4
Identification
ColorBlack, brownish-black
Crystal habitMassive, compact; acicular, may be minutely spherical.
CleavageNone
FractureConchoidal
TenacityBrittle
Mohs scale hardness2.5 - 3.0
LusterVitreous, resinous, greasy
StreakYellowish brown, green
DiaphaneityTransparent to translucent
Specific gravity2.43 - 2.67
Optical propertiesBiaxial (-)
Refractive indexnα = 1.715 nγ = 1.730
Birefringenceδ = 0.015
References

Hisingerite is an iron(III) phyllosilicate mineral with formula FeIII2Si2O5(OH)4 · 2 H2O. A black or dark brown, lustrous secondary mineral, it is formed by the weathering or hydrothermal alteration of other iron silicate and sulfide minerals.

It was first described in 1751 by A.F. Cronstedt from Väster Silvberg, Dalarna, Sweden (under the name “kolspeglande järnmalm”), and in 1810 by W. Hisinger from the Gillinge iron mine, Södermanland, Sweden (“svart stenart”, later “gillingit”). In 1828 it was found at an occurrence in Riddarhyttan, Vastmanland, Sweden. It was named after Wilhelm Hisinger (1766–1852), a Swedish chemist.

There are also aluminian hisingerite variety in which one of the iron atoms is replaced by aluminium and chrome-alumina-hisingerite variety in which chromium substitutes for iron.



This page was last updated at 2023-10-30 20:12 UTC. Update now. View original page.

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