Geigerite
General
CategoryArsenate minerals
Formula
(repeating unit)		Mn5(AsO3OH)2(AsO4)2·10H2O
IMA symbolGga[1]
Strunz classification8.CE.05
Crystal systemTriclinic
Crystal classPinacoidal (1)
(same H-M symbol)
Space groupP1
Unit cella = 7.94 Å, b = 10.69 Å
c = 6.77 Å; α = 80.97°
β = 84.2°, γ = 81.85°; Z = 1
Identification
Formula mass1,012.54 g/mol
ColorRed, colorless
Crystal habitPlaty, partly triangular crystals to 0.5 mm
CleavagePerfect
Tenacitybrittle
Mohs scale hardness3
LusterVitreous – pearly
StreakWhite
DiaphaneityTransparent to translucent
Specific gravity3.05
Optical propertiesBiaxial (−)
Refractive indexnα = 1.601 nβ = 1.630 nγ = 1.660
Birefringenceδ = 0.059
PleochroismVery weak, colorless to rose-red
2V angle89°
References[2][3][4][5]

Geigerite is a mineral, a complex hydrous manganese arsenate with formula: Mn5(AsO3OH)2(AsO4)2·10H2O. It forms triclinic pinacoidal, vitreous, colorless to red to brown crystals. It has a Mohs hardness of 3 and a specific gravity of 3.05.[2][3]

It was discovered in Grischun, Switzerland in 1989. It was named in honor of Thomas Geiger (1886–1976), Wiesendangen, Switzerland, who studied the Falotta manganese ores.[5][6]

Composition

The chemical composition of geigerite is hydrous manganese arsenate (Mn5(AsO3OH)2(AsO4)2·10H2O).[4] The chemical composition was found by using an electron microprobe in the Falotta mines in Switzerland.[4]

Geologic occurrence

Geigerite can be found in the abandoned manganese mine in Oberhalbstein, Switzerland. It is mainly found in cavities in adiolarites, which are a form of igneous rock that have either a radial or fanlike texture of crystals. Geigerite is then formed by metamorphism of manganese oxide ores.[4] Recently, geigerite has been found in Fukushima Prefecture, Japan.[7] Geigerite has also been found in Mt. Nero Mine, Borghetto Di Vara, La Spieza, Italy.[8]

Structure

Geigerite’s crystal system is triclinic with perfect cleavage on the {010}. The Herman Mauguin symbol for geigerite is 1 and its space group is P1.[2] Geigerite contains two arsenate ions which are independent of one another. The first is the AsO3OH group, and the second is the AsO4. In the acidic AsO3OH group, the As-O bonds are much shorter than the As-OH bonds. Similarly, in the AsO4 group, As-O bonds are also shorter than the As-O bonds. The remaining bonds within both arsenate groups have nearly equal distances. In the ions there are three manganese atoms, these three links to six oxygen atoms to form a normal octahedral formation.[4]

Special characteristics

One interesting structural feature of geigerite is the presence of a complicated network of hydrogen bonds, which exceed the number of the hydrogen atoms.[4] Geigerite is classified under a group of metal copper (II) arsenates called the Lindackerite group. Minerals within this group have a formula where M equals either copper, calcium, manganese, zinc, or cobalt.[9]

See also

References

  1. ↑ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
  2. 1 2 3 Geigerite data on Webmineral.com
  3. 1 2 Geigerite on Mindat.org
  4. 1 2 3 4 5 6 Graeser, S.; Schwander, H.; Bianchi, R.; Pilati, T.; Gramaccioli, C. M. (1989): Geigerite, the manganese analogue of chudobaite: Its description and crystal structure. American Mineralogist: 74, 676–684.
  5. 1 2 Geigerite in the Handbook of Mineralogy
  6. ↑ Geiger, Thomas (1948). Manganerze in der Radiolariten Graubündens (PDF) (Ph.D.). ETH Zürich.
  7. ↑ Kato et al. (1990) Ganseki-Koubutsu-Koshogaku Zasshi, 85, 184.; Mineralogical Journal Vol. 18 (1996), No. 4 pp 155–160
  8. ↑ Cabella, R. (2000) Geigerite from Mt Nero manganese mine (Northern Apennines, La Spezia, Italy). Neues Jahrbuch fur Mineralogy-Monatshefte, 570–576.
  9. ↑ Hybler, M. (2003) Crystal structure of Lindackerite, (Cu,Co,Ni)CU4(AsO4)(2)(AsO3OH)(2)center dot 9 H2O from Jachymov, Czech republic. European Journal of Mineralogy, 1035–1042.
  • Bergknappe (2000) Verein der Freunde des Bergbaus in Graubunden Stiftung Bergbaumuseum Graubunden Schelzboden-Davos. 31–32.


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