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Genèvéite

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Formula:
(Cu,Zn)9(AsO4)2(OH)12 · 2H2O
Colour:
blue-green
Lustre:
Vitreous
Specific Gravity:
3.45
Crystal System:
Hexagonal
Name:
Named after the city of Genève.
Probably identical to Theisite.

Originally described from Tyrol, Austria.
Never submitted to the IMA, but name published nonetheless.


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Name EncodingHide

ASCII-7:
Geneveite

Unique IdentifiersHide

Mindat ID:
10264
Long-form identifier:
mindat:1:1:10264:1

Similar NamesHide

GeneviteA synonym of Vesuvianite

Physical Properties of GenèvéiteHide

Vitreous
Colour:
Blue-green
Density:
3.45 g/cm3 (Measured)    4.19 g/cm3 (Calculated)

Chemistry of GenèvéiteHide

Mindat Formula:
(Cu,Zn)9(AsO4)2(OH)12 · 2H2O
Element Weights:
Element% weight
Cu52.475 %
O32.296 %
As13.749 %
H1.480 %

Calculated from ideal end-member formula.

Crystallography of GenèvéiteHide

Crystal System:
Hexagonal
Class (H-M):
6mm - Dihexagonal Pyramidal
Space Group:
P6mm
Cell Parameters:
a = 8.26 Å, c = 14.7 Å
Ratio:
a:c = 1 : 1.78
Unit Cell V:
868.58 ų (Calculated from Unit Cell)
Z:
2

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
14.69 Å(35)
7.35 Å(50)
4.117 Å(35)
3.672 Å(60)
2.530 Å(100)
2.172 Å(30)
1.810 Å(35)
1.557 Å(30)

Other Language Names for GenèvéiteHide

German:Genevéit
Spanish:Genevéita

Other InformationHide

Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.

Internet Links for GenèvéiteHide

References for GenèvéiteHide

Localities for GenèvéiteHide

Showing 1 localities.

ⓘ - Click for references and further information on this occurrence. ? - Indicates mineral may be doubtful at this locality. - Good crystals or important locality for species. - World class for species or very significant. (TL) - Type Locality for a valid mineral species. (FRL) - First Recorded Locality for everything else (eg varieties). Struck out - Mineral was erroneously reported from this locality. Faded * - Never found at this locality but inferred to have existed at some point in the past (e.g. from pseudomorphs).

All localities listed without proper references should be considered as questionable.
Austria
 
Sarp et al. (1983)
 
and/or  
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