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Seraphinite

From Wikipedia, the free encyclopedia
Seraphinite
Seraphinite specimen
General
CategoryPhyllosilicate minerals
GroupChlorite group
Formula(Mg, Fe3+Al(Si3Al)O10(OH)8
Crystal systemMonoclinic
Identification
Colorgreen, white, colourless
Mohs scale hardness2–2.5
LusterPearly, dull, greasy
Streaklight green
Diaphaneitytransparent, translucent to opaque
Specific gravity2.600–3.000
Optical propertiesBiaxial (–)
Refractive index1.571–1.597
Birefringence0.005–0.011
Ultraviolet fluorescenceinert

Seraphinite is a trade name for a particular form of clinochlore, a member of the chlorite group.

Seraphinite apparently acquired its name due to its resemblance to feathers due to its chatoyancy. Seraphinite is named after the biblical seraphs or seraphim angels.[1] With some specimens the resemblance is quite strong, with shorter down-like feathery growths leading into longer "flight feathers"; the resemblance even spurs fanciful marketing phrases like "silver plume seraphinite." Seraphinite is generally dark green to gray in color, has chatoyancy, and has hardness between 2 and 4 on the Mohs scale of mineral hardness.

Seraphinite is mined in a limited area of eastern Siberia in Russia. Russian mineralogist Nikolay Koksharov (1818-1892 or 1893) is often credited with its discovery. It occurs in the Korshunovskoye iron skarn deposit in the Irkutskaya Oblast of Eastern Siberia.[2]

References

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