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Zinkosite

A valid IMA mineral species - grandfathered - questionable
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Formula:
ZnSO4
Specific Gravity:
4.33
Crystal System:
Orthorhombic
Probably an artificial product, and its occurence in nature (at least at its "type locality") is doubtful (Calvo and Viñals, 2008).


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Unique IdentifiersHide

Mindat ID:
4418
Long-form identifier:
mindat:1:1:4418:5

Similar NamesHide

Native ZincA valid IMA mineral species - grandfatheredZn
SincositeA valid IMA mineral species - grandfatheredCa(V4+O)2(PO4)2 · 4H2O
ZinciteA valid IMA mineral species - grandfatheredZnO
ZinkeniteA valid IMA mineral species - grandfatheredPb9Sb22S42

IMA Classification of ZinkositeHide

Approved, 'Grandfathered' (first described prior to 1959), Questionable
IMA Formula:
Zn2+S6+O4

Classification of ZinkositeHide

7.AB.10

7 : SULFATES (selenates, tellurates, chromates, molybdates, wolframates)
A : Sulfates (selenates, etc.) without additional anions, without H2O
B : With medium-sized cations
25.5.1

25 : Sulphates
5 : Sulphates of Zn and 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
ZinIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43

Physical Properties of ZinkositeHide

Transparency:
Translucent
Density:
4.33 g/cm3 (Measured)    3.86 g/cm3 (Calculated)

Optical Data of ZinkositeHide

Type:
Biaxial (-)
RI values:
nα = 1.658 nβ = 1.669 nγ = 1.67
2V:
Measured: 25° , Calculated: 32°
Max. Birefringence:
δ = 0.012
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:
strong

Chemistry of ZinkositeHide

Mindat Formula:
ZnSO4
Element Weights:
Element% weight
Zn40.497 %
O39.641 %
S19.862 %

Calculated from ideal end-member formula.
Zn
O
S

Crystallography of ZinkositeHide

Crystal System:
Orthorhombic
Class (H-M):
mmm(2/m2/m2/m) - Dipyramidal
Space Group:
Pnma
Setting:
Pnma
Cell Parameters:
a = 8.604(5) Å, b = 6.746(5) Å, c = 4.774(3) Å
Ratio:
a:b:c = 1.275 : 1 : 0.708
Unit Cell V:
277.10 ų (Calculated from Unit Cell)
Z:
4

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0014620ZinkositeWildner M, Giester G (1988) Crystal structure refinements of synthetic chalcocyanite (CuSO4) and zincosite (ZnSO4) Mineralogy and Petrology 39 201-2091988synthetic0293
0009208ZinkositeKokkoros P A, Rentzeperis P J (1958) The crystal structure of the anhydrous sulphates of copper and zinc Acta Crystallographica 11 361-36419580293
CIF Raw Data - click here to close

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 7: Great Oxidation Event<2.4
47b : [Sulfates and sulfites]
47h : [Near-surface oxidized, dehydrated minerals]

Type Occurrence of ZinkositeHide

Synonyms of ZinkositeHide

Other Language Names for ZinkositeHide

Related Minerals - Strunz-mindat GroupingHide

7.AB.DravertiteCuMg(SO4)2Mon. 2/m
7.AB.AndymcdonalditeFe2TeO6Tet. 4/mmm(4/m2/m2/m) : P42/mnm
7.AB.DagenaisiteZn3Te6+O6Mon. 2/m : B2/b
7.AB.05MikasaiteFe2(SO4)3Trig. 3 : R3
7.AB.05MillosevichiteAl2(SO4)3Trig. 3 : R3
7.AB.05KoryakiteNaKMg2Al2(SO4)6Trig. 3 : R3
7.AB.10ChalcocyaniteCuSO4Orth. mmm(2/m2/m2/m)
7.AB.15HermannjahniteCuZn(SO4)2Mon. 2/m
7.AB.25OttoitePb2TeO5Mon. 2/m : B2/b
7.AB.55McalpineiteCu3(Te6+O6)Iso. m3(2/m3) : Ia3

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 ZinkositeHide

References for ZinkositeHide

Localities for ZinkositeHide

Showing 6 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.
China
 
  • Guangdong
    • Shaoguan
      • Renhua Co.
Zhongjing Lingnan Nonferrous Metals Data
Spain (TL)
 
  • Andalusia
    • Almería
      • Cuevas del Almanzora
        • Sierra Almagrera
AM 45 (1960)
Tunisia
 
  • Zaghouan
Somrani et al. (2025)
    • Zriba-Village
Somrani et al. (2025)
USA
 
  • New Mexico
    • Socorro County
Northrop et al. (1996)
Northrop et al. (1996)
 
and/or  
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