Avogadrite
| Avogadrite | |
|---|---|
 Ferruccite (white) on avogadrite (yellow-brownish), picture size: 5 mm | |
| General | |
| Category | Halide mineral |
| Formula (repeating unit) | (K,Cs)BF4 |
| Strunz classification | 3.CA.10 |
| Crystal system | Orthorhombic |
| Crystal class | Dipyramidal (mmm) H-M symbol: (2/m 2/m 2/m) |
| Space group | Pnma |
| Unit cell | a = 8.6588, b = 5.48 c = 7.0299 [Å]; Z = 4 |
| Identification | |
| Color | Colorless to white, yellowish to reddish |
| Crystal habit | Tabular to platy octagonal crystals |
| Luster | Vitreous, greasy |
| Diaphaneity | Translucent |
| Specific gravity | 2.9 |
| Optical properties | Biaxial (-) |
| Refractive index | nα = 1.3239, nβ = 1.3245, nγ = 1.3247 |
| Birefringence | δ = 0.001 |
| 2V angle | 75°(meas), 58° (calc) |
| References | [1][2][3] |
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.
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. As a result, it can only found as a sublimation product around volcanic fumaroles.[1] He named it after the Italian scientist Amedeo Avogadro (1776–1856).[4]
See also
- Ferruccite, (NaBF4), the sodium tetrafluoroborate.
References
- ^ a b "Handbook of Mineralogy: Avogadrite" (PDF). The Mineralogical Society of America. Retrieved 2010-01-09.
- ^ Avogadrite on Mindat.org
- ^ Avogadrite data on Webmin
- ^ Zambonini, Ferruccio (1926). "Sulla presenza, tra i prodotti dell'attuale attività del Vesuvio, di una varietà cesifera del fluoborato di potassio, (On the presence, among the products of Vesuvius, of a caesium-bearing variety of potassium fluoborate), Rend. Accad. Lincei". 6 (III): 644–649.
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