Avogadrite

Halide mineral From Wikipedia, the free encyclopedia

Avogadrite ((K,Cs)BF4) is a potassium-caesium tetrafluoroborate in the halide class. Avogadrite crystallizes in the orthorhombic system (space group Pnma) with cell parameters a 8.66 Å, b 5.48 Å and c Å 7.03.

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Avogadrite
Ferruccite (white) on avogadrite (yellow-brownish), picture size: 5 mm
General
CategoryHalide mineral
Formula(K,Cs)BF4
IMA symbolAvg[1]
Strunz classification3.CA.10
Crystal systemOrthorhombic
Crystal classDipyramidal (mmm)
H-M symbol: (2/m 2/m 2/m)
Space groupPnma
Unit cella = 8.6588, b = 5.48
c = 7.0299 [Å]; Z = 4
Identification
ColorColorless to white, yellowish to reddish
Crystal habitTabular to platy octagonal crystals, tiny crystals, elongate
LusterVitreous, greasy
DiaphaneityTranslucent
Specific gravity2.9
Optical propertiesBiaxial (-)
Refractive indexnα = 1.3239, nβ = 1.3245, nγ = 1.3247
Birefringenceδ = 0.001
2V angle75°(meas), 58° (calc)
Other characteristicsBitter taste
References[2][3][4]
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History

The mineral was discovered by the Italian mineralogist Ferruccio Zambonini in 1926. He analyzed several samples from the volcanic fumaroles close to Mount Vesuvius and from the Lipari islands. In nature, it can only be found as a sublimation product around volcanic fumaroles.[2] He named it after the Italian scientist Amedeo Avogadro (1776–1856).[5]

Bibliography

  • Palache, P.; Berman H.; Frondel, C. (1960). "Dana's System of Mineralogy, Volume II: Halides, Nitrates, Borates, Carbonates, Sulfates, Phosphates, Arsenates, Tungstates, Molybdates, Etc. (Seventh Edition)" John Wiley and Sons, Inc., New York, pp. 97-98.

References

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