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Warikahnite

A valid IMA mineral species
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About WarikahniteHide

Formula:
Zn3(AsO4)2 · 2H2O
Colour:
Colourless to light yellow
Lustre:
Vitreous, Waxy
Hardness:
2
Specific Gravity:
4.24
Crystal System:
Triclinic
Name:
Named after Walter Richard Kahn (22 April 1911 in Braunlage, Germany, † 14 May 2009 in Bad Bayersoien, Germany), dealer and collector specializing in Tsumeb minerals, for his financial support of research on secondary minerals and their crystal structures.
Note: Some "warikahnites" (yellow prisms associated with Cu-bearing adamite and olivenite sprays) recently (late 1980s and later) sold turned out to be willemites. This material is similar to that shown in http://www.mindat.org/photo-174225.html and http://www.mindat.org/photo-372025.html .


Unique IdentifiersHide

Mindat ID:
4244
Long-form identifier:
mindat:1:1:4244:0

IMA Classification of WarikahniteHide

Classification of WarikahniteHide

8.CA.35

8 : PHOSPHATES, ARSENATES, VANADATES
C : Phosphates without additional anions, with H2O
A : With small and large/medium cations
40.3.1.1

40 : HYDRATED NORMAL PHOSPHATES,ARSENATES AND VANADATES
3 : A3(XO4)2·xH2O
20.3.5

20 : Arsenates (also arsenates with phosphate, but without other anions)
3 : Arsenates of Zn, Cd or Hg

Mineral SymbolsHide

As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.

SymbolSourceReference for Standard
WarIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43

Physical Properties of WarikahniteHide

Vitreous, Waxy
Transparency:
Transparent
Colour:
Colourless to light yellow
Streak:
White
Hardness:
Cleavage:
Perfect
{001} perfect, {010} and [l0O] distinct to good.
Density:
4.24 g/cm3 (Measured)    4.29 g/cm3 (Calculated)

Optical Data of WarikahniteHide

Type:
Biaxial (+)
RI values:
nα = 1.747 nβ = 1.753 nγ = 1.768
2V:
Measured: 75° , Calculated: 66°
Max. Birefringence:
δ = 0.021
Based on recorded range of RI values above.

Interference Colours:
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.

Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.

Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.

Surface Relief:
Very High (positive)
Relative to Canada balsam mounting medium (n ≈ 1.537).

This shows the grain boundary and Becke line effect under plane-polarised light, based on the contrast between this mineral's average refractive index and the mounting medium. It does not take into account mineral colouration.
In focus
Interference Figure:
This shows the idealized biaxial acute bisectrix (Bxa) interference figure - the conoscopic view for a grain cut perpendicular to the acute bisectrix, using this mineral's 2V. The two small white dots mark the melatopes - the points where the two optic axes emerge - and are shown only when they fall within the field of view. The coloured bands are isochromatics, and the dark bands are isogyres.

Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.
Dispersion:
r > v, (type description says none observed)
Optical Extinction:
Z ∧ a = 47° on {010}; OAP ≃ {001}.

Chemistry of WarikahniteHide

Mindat Formula:
Zn3(AsO4)2 · 2H2O
Element Weights:
Element% weight
Zn38.458 %
O31.371 %
As29.381 %
H0.791 %

Calculated from ideal end-member formula.
Zn
O
As
H

Crystallography of WarikahniteHide

Crystal System:
Triclinic
Class (H-M):
1 - Pinacoidal
Space Group:
P1
Cell Parameters:
a = 6.71 Å, b = 8.98 Å, c = 14.53 Å
α = 105.59°, β = 93.44°, γ = 108.68°
Ratio:
a:b:c = 0.747 : 1 : 1.618
Unit Cell V:
788.58 ų (Calculated from Unit Cell)
Z:
4
Morphology:
Bladed subhedral crystals, elongated along [100], flattened on {010}, and striated. Forms include {010}, {100}, {001}, and {0kl}.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0015678WarikahniteRiffel H, Keller P, Hess H (1980) Die kristallstruktur von warikahnit, Zn3[(H2O)2|(AsO4)2] Tschermaks Mineralogische und Petrographische Mitteilungen 27 187-1991980Tsumeb mine, Namibia0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
8.12 Å(60)
6.21 Å(80)
3.45 Å(70)
3.04 Å(60)
2.87 Å(80)
2.82 Å(100)
2.30 Å(70)

Geological EnvironmentHide

Paragenetic Mode(s):

Type Occurrence of WarikahniteHide

General Appearance of Type Material:
Crystals are bladed, up to 3 x 0.5 x 0.5 mm, elongated on [100], in radiating masses.
Place of Conservation of Type Material:
University of Stuttgart, Stuttgart, Germany, number NM04.
Harvard University, Cambridge, Massachusetts, USA, numbers 117116, 117117.
National Museum of Natural History, Washington, D.C., USA, numbers 144801, 144802, 147462.
Geological Setting of Type Material:
On corroded tennantite.
Associated Minerals at Type Locality:

Synonyms of WarikahniteHide

Other Language Names for WarikahniteHide

Common AssociatesHide

Associations Based on Photo Data:
2 photos of Warikahnite associated with LeiteiteZn(As2O4)
1 photo of Warikahnite associated with KoritnigiteZn(AsO3OH) · H2O
1 photo of Warikahnite associated with Tennantite-(Zn)Cu6(Cu4Zn2)As4S12S

Related Minerals - Strunz-mindat GroupingHide

8.CA.ApexiteNaMg(PO4) · 9H2OTric. 1 : P1
8.CA.BrandãoiteBeAl2(PO4)2(OH)2(H2O)5Tric. 1 : P1
8.CA.DavidlloyditeZn3(AsO4)2 · 4H2OTric. 1 : P1
8.CA.05ParafransoletiteCa3Be2(PO4)2(PO3OH)2 · 4H2OTric. 1 : P1
8.CA.05FransoletiteCa3Be2(PO4)2(PO3OH)2 · 4H2OMon. 2/m : P21/c
8.CA.10EhrleiteCa4Be3Zn2(PO4)6 · 9H2OTric. 1 : P1
8.CA.15FaheyiteBe2Mn2+Fe3+2(PO4)4 · 6H2OTrig. 32 : P3121
8.CA.20MccrillisiteNaCs(Be,Li)Zr2(PO4)4 · 1-2H2OTet. 4/mmm(4/m2/m2/m) : I41/amd
8.CA.20GainesiteNa(Na,K)(Be,Li)Zr2(PO4)4 · 1.5-2H2OTet. 4mm : I41md
8.CA.20SelwyniteNaK(Be,Al)Zr2(PO4)4 · 2H2OTet. 4/mmm(4/m2/m2/m) : I41/amd
8.CA.25PahasapaiteLi8(Ca,Li,K)10.5Be24(PO4)24 · 38H2OIso. 23 : I23
8.CA.30NizamoffiteMn2+Zn2(PO4)2(H2O)4Orth. mmm(2/m2/m2/m) : Pbcm
8.CA.30ArsenohopeiteZn3(AsO4)2 · 4H2OOrth. mmm(2/m2/m2/m) : Pnma
8.CA.30HopeiteZnZn2(PO4)2 · 4H2OOrth. mmm(2/m2/m2/m) : Pnma
8.CA.40PhosphophylliteZn2Fe 2+(PO4)2 · 4H2OMon. 2/m : P21/c
8.CA.42SteinmetziteZn2Fe3+(PO4)2(OH) · 3H2OTric. 1 : P1
8.CA.45ParascholziteCaZn2(PO4)2 · 2H2OMon.
8.CA.45ScholziteCaZn2(PO4)2 · 2H2OOrth. mmm(2/m2/m2/m) : Pbcm
8.CA.50KeyiteCu2+3Zn4Cd2(AsO4)6 · 2H2OMon. 2/m : B2/b
8.CA.55PushcharovskiteK0.6Cu18[AsO2(OH)2]4[AsO3OH]10(AsO4)(OH)9.6 · 18.6H2OTric.
8.CA.60ProsperiteCa2Zn4(AsO4)4 · H2OMon.
8.CA.65GengenbachiteKFe3+3(PO3OH)4[PO2(OH)2]2 · 6H2OTrig. 3m : P31c
8.CA.70ParahopeiteZn3(PO4)2 · 4H2OTric. 1 : P1
8.CA.70ReaphookhilliteMgZn2(PO4)2 · 4H2OTric. 1 : P1
8.CA.75StergiouiteCaZn2(AsO4)2 · 4H2OMon. m : Pb
8.CA.80LimousiniteBaCa[Be4P4O16] · 6H2OMon. 2/m : P21/c
8.CA.85MinjiangiteBaBe2(PO4)2Hex. 6/mmm(6/m2/m2/m) : P6/mmm
8.CA.85Wilancookite(Ba5Li2◻)Ba6Be24P24O96 · 26H2OIso. 23 : I23

Other InformationHide

IR Spectrum:
Shows the presence of H2O and (AsO4)3-.
Thermal Behaviour:
Water loss occurs in one step at 365 °C.
Notes:
Dissolved by hot HCl or HNO3.
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 WarikahniteHide

References for WarikahniteHide

Localities for WarikahniteHide

Showing 4 localities.

This map shows a selection of localities that have latitude and longitude coordinates recorded. Click on the symbol to view information about a locality. The symbol next to localities in the list can be used to jump to that position on the map.
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Locality ListHide

- This locality has map coordinates listed. - This locality has estimated coordinates. ⓘ - 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.
Greece
 
  • Attica
    • East Attica
      • Lavreotiki
        • Agios Konstantinos (Kamariza)
          • Mercati mines
Rieck (1999)
        • Plaka
          • Plaka Mines
Pinch (2005)
Namibia (TL)
 
  • Oshikoto Region
    • Tsumeb
Keller et al. (1979) +1 other reference
 
and/or  
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