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Sigogglinite

A valid IMA mineral species
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About SigoggliniteHide

Formula:
[Pb6Zn(OH)8]2(SO4)6 · (H2O)8-x
0 ≤ x ≤ 1
Colour:
colourless
Lustre:
Vitreous, Waxy
Hardness:
3
Specific Gravity:
5.085 - 5.107
Crystal System:
Monoclinic
Name:
For the Appalachian English slang term “sigogglin”, which has a general meaning along the lines of tilted, skewed, winding, ‘not right’, or not built correctly. This is a reference to several aspects of the mineral’s appearance and crystal structure.
A very rare Pb-Zn sulfate mineral with cubane-like structural units topologically related to those of redmondite, hydroredmondite, and sulfatoredmondite.

Two polytypoids are known: sigogglinite-P2/n (7 H2O per formula unit) and sigogglinite-P21/c (8 H2O per formula unit).


Unique IdentifiersHide

Mindat ID:
471929
Long-form identifier:
mindat:1:1:471929:4

IMA Classification of SigoggliniteHide

Approved
IMA Formula:
[Pb2+6Zn2+(OH)8](S6+O4)3·3H2O
Approval year:
2024
Approval history:
IMA2024-069

Classification of SigoggliniteHide

7.DF.

7 : SULFATES (selenates, tellurates, chromates, molybdates, wolframates)
D : Sulfates (selenates, etc.) with additional anions, with H2O
F : With large and medium-sized cations

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

Physical Properties of SigoggliniteHide

Vitreous, Waxy
Transparency:
Transparent
Colour:
Colourless
Streak:
White
Hardness:
Hardness Data:
Measured
Comment:
Based on scratch tests
Tenacity:
Brittle
Cleavage:
Distinct/Good
Good on {100} (P2/n); equivalent to {001} in P21/c polytypoid.
Fracture:
Irregular/Uneven
Density:
5.085 - 5.107 g/cm3 (Measured)    
Comment:
Calculated. Lower density is for P2/n, higher density is for P2(1)/c.

Optical Data of SigoggliniteHide

Type:
Biaxial (-)
RI values:
nα = 1.754(3) nβ = 1.768(3) nγ = 1.772(3)
2V:
Measured: 50.9° (4)
Max. Birefringence:
δ = 0.018
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 weak
Orientation:
Z = b, Y ^ c = 28° in obtuse angle β
Pleochroism:
Non-pleochroic

Chemistry of SigoggliniteHide

Mindat Formula:
[Pb6Zn(OH)8]2(SO4)6 · (H2O)8-x

0 ≤ x ≤ 1
Element Weights:
Element% weight
Pb69.574 %
O20.594 %
S5.383 %
Zn3.659 %
H0.790 %

Calculated from ideal end-member formula.
Pb
O
S
Zn
H

Crystallography of SigoggliniteHide

Polytype:
Formula:
Crystal System:
Class (H-M)
Space Group:
Space Group Setting:
Cell Parameters:
Ratio:
Unit Cell Volume (calc):
Z:
Comment:
Sigogglinite-P2(1)/cSigogglinite-P2/n
[Pb6Zn(OH)8]2(SO4)6 · (H2O)8[Pb6Zn(OH)8]2(SO4)6 · (H2O)7
Monoclinic Monoclinic 
2/m - Prismatic2/m - Prismatic
P21/cP2/c
P21/cP2/m
a = 9.0243(2) Å, b = 17.6454(3) Å, c = 14.8646(3) Å
β = 95.166(1)°
a = 14.8109(2) Å, b = 9.1360(1) Å, c = 17.3693(3) Å
β = 92.879(1)°
a:b:c = 0.511 : 1 : 0.842a:b:c = 1.621 : 1 : 1.901
V 2357.39 ųV 2347.31 ų
22
 P2/n

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
7.349 Å(76)
5.854 Å(100)
3.800 Å(82)
3.535 Å(83)
2.946 Å(67)
2.907 Å(54)
2.781 Å(58)
2.580 Å(56)

Type Occurrence of SigoggliniteHide

General Appearance of Type Material:
Stout six-sided tablets with diagonal striations (P2/n polytype) or as a lone reticulated lathe-like crystal (P2(1)/c polytype)
Place of Conservation of Type Material:
Type material is deposited in the collections of the Natural History Museum of Los Angeles County, 900 Exposition Boulevard, Los Angeles, CA 90007, USA, catalogue number 76449
Geological Setting of Type Material:
Supergene zone of a small lead-zinc vein hosted within metamorphic rocks.

Synonyms of SigoggliniteHide

Other Language Names for SigoggliniteHide

Related Minerals - Strunz-mindat GroupingHide

7.DF.Siligiite[Pb(H2O)5(SO4)][Zn9(OH)18]Mon. 2/m : P21/c
7.DF.AlcaparrosaiteK3Ti4+Fe3+(SO4)4O(H2O)2Mon. 2/m : B2/b
7.DF.FlaggitePb4Cu2+4Te6+2(SO4)2O11(OH)2(H2O)Tric. 1 : P1
7.DF.BairditePb2Cu2+4Te6+2O10(OH)2(SO4) · H2OMon. 2/m : P21/c
7.DF.TzeferisiteCaZn8(SO4)2(OH)12Cl2(H2O)9Trig. 3m(32/m) : R3c
7.DF.Cherokeeite[Pb2Zn(OH)4](SO4) · H2OMon. 2/m : P21/c
7.DF.Ammoniomathesiusite(NH4)5(UO2)4(SO4)4(VO5) · 4H2OTet. 4/m : P4/n
7.DF.XBlueridgeite[Pb8Zn3Cu2+(OH)16](SO4)2(S2O3)2 · 2H2OMon. 2/m : P21/c
7.DF.ErssoniteMg7Fe3+2(OH)18[Ca(H2O)6](SO4)2 · 12H2OTrig. 3m(32/m) : P3c1
7.DF.PoellmanniteCa6Al3(OH)18[Na(H2O)6](SO4)2 · 6H2OTrig. 3 : R3
7.DF.Carlsonite(NH4)5Fe3+3O(SO4)6 · 7H2OTric. 1 : P1
7.DF.Cuprocherokeeite[Pb8Zn3Cu2+(OH)16](SO4)4 · 4H2OMon. 2/m : P21/c
7.DF.Haywoodite[Pb(H2O)10][Zn12(OH)20(H2O)(SO4)3]Tric. 1 : P1
7.DF.ChromschieffelinitePb10Te6+6O20(OH)14(CrO4)(H2O)5Orth. 222 : C2221
7.DF.05UklonskoviteNaMg(SO4)F · 2H2OMon. 2/m : P21/m
7.DF.10KainiteKMg(SO4)Cl · 3H2OMon. 2/m : B2/m
7.DF.10KaliochalciteKCu2(SO4)2[(OH)(H2O)]Mon. 2/m : B2/m
7.DF.15NatrochalciteNaCu2(SO4)2(OH) · 2H2OMon. 2/m : B2/m
7.DF.17GenplesiteCa3Sn(SO4)2(OH)6 · 3H2OHex. 6/mmm(6/m2/m2/m) : P63/mmc
7.DF.17'Unnamed (Ba-Sb Silicate-Sulphate-Hydroxide-Hydrate)'Ba3Sb5+[(Si,S)O3(OH)]2(OH,O)6 · 3H2O Trig. 3 : P3
7.DF.20SideronatriteNa2Fe(SO4)2(OH) · 3H2OOrth. 222 : P212121
7.DF.20MetasideronatriteNa2Fe(SO4)2(OH) · H2OOrth. mmm(2/m2/m2/m) : Pnma
7.DF.25FleischeritePb3Ge(SO4)2(OH)6 · 3H2OHex. 6/mmm(6/m2/m2/m) : P63/mmc
7.DF.25MallestigitePb3Sb5+(SO4)(AsO4)(OH)6 · 3H2OHex. 6 : P63
7.DF.25SchaurteiteCa3Ge(SO4)2(OH)6 · 4H2OHex. 6/mmm(6/m2/m2/m) : P63/mmc
7.DF.25DespujolsiteCa3Mn4+(SO4)2(OH)6 · 3H2OHex. 6m2 : P62c
7.DF.30Slavíkite(H3O+)3Mg6Fe15(SO4)21(OH)18 · 98H2OTrig. 3 : R3
7.DF.35MetavoltineK2Na6Fe2+Fe3+6O2(SO4)12 · 18H2OTrig.
7.DF.40LannoniteMg2Ca4Al4(SO4)8F8 · 24H2OTet. 4/m : I4/m
7.DF.40VlodavetsiteAlCa2(SO4)2F2Cl · 4H2OTet. 4/m : I4/m
7.DF.45PeretaiteCa(SbO)4(SO4)2(OH)2 · 2H2OMon. 2/m : B2/b
7.DF.50GordaiteNaZn4(SO4)(OH)6Cl · 6H2OTrig. 3 : P3
7.DF.50CalamaiteNa2TiO(SO4)2 · 2H2OOrth. mmm(2/m2/m2/m) : Ibam
7.DF.52Huizingite-(Al)[(NH4)9(SO4)2][(Al,Fe3+)3(OH)2(H2O)4(SO4)6]Tric. 1 : P1
7.DF.52ScordariiteK8(Fe3+0.67◻0.33)[Fe3+3O(SO4)6]2 · 14H2OTrig. 3 : R3
7.DF.55Clairite(NH4)2Fe3(SO4)4(OH)3 · 3H2OTric.
7.DF.55GiacovazzoiteK5Fe3+3O(SO4)6 · 10H2OMon. 2/m : P21/c
7.DF.57MagnanelliiteK3Fe3+2(SO4)4(OH)(H2O)2Mon. 2/m : B2/b
7.DF.60ArzruniteCu4Pb2(SO4)(OH)4Cl6 · 2H2O (?)Orth.
7.DF.60EvdokimoviteTl4(VO)3(SO4)5(H2O)5Mon. 2/m : P21/c
7.DF.62Bridgesite-(Ce)CaCe2Cu6(SO4)4(OH)12 · 8H2OMon. 2/m : B2/m
7.DF.65ElyitePb4Cu(SO4)O2(OH)4 · H2OMon. 2/m : P21/c
7.DF.70YecoraiteFe3+3Bi5(Te6+O4)2(Te4+O3)O9 · 9H2O
7.DF.70LautenthalitePbCu4(SO4)2(OH)6 · 3H2OMon. 2/m : P21/c
7.DF.75RiomarinaiteBi(SO4)(OH) · H2OMon. 2/m : P21/c
7.DF.80DukeiteBi3+24Cr6+8O57(OH)6 · 3H2OTrig. 3m : P31c

Fluorescence of SigoggliniteHide

Non-fluorescent

Other InformationHide

Magnetism:
Non-Magnetic
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 SigoggliniteHide

References for SigoggliniteHide

Localities for SigoggliniteHide

Showing 3 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.
USA (TL)
 
  • North Carolina
    • Haywood County
      • Waterville Lake
[Sigogglinite-P2(1)/c, Sigogglinite-P2/n] Bosi et al. (2025)
 
and/or  
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