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Gerstmannite

A valid IMA mineral species
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About GerstmanniteHide

01299140017271923508112.jpg
Ewald Gerstmann
Formula:
MnMgZn(SiO4)(OH)2
Colour:
White to very pale pink.
Lustre:
Sub-Adamantine, Vitreous, Silky
Hardness:
Specific Gravity:
3.68
Crystal System:
Orthorhombic
Name:
Named in 1977 by Paul Brian Moore and Takaharu Araki after Mr. Ewald "The Dutchman" Gerstmann [September 19, 1918 in Bremerhaven, Germany - December 14, 2005, Andover, New Jersey], stationary engineer, mineral dealer, and avid collector of Franklin Mining District minerals. Operator of a private mineral museum and collectors' gathering spot at Franklin, NJ, for many years. The Gerstmann mineral collection was donated to the Franklin Mineral Museum.
This page provides mineralogical data about Gerstmannite.


Unique IdentifiersHide

Mindat ID:
1685
Long-form identifier:
mindat:1:1:1685:4

IMA Classification of GerstmanniteHide

Classification of GerstmanniteHide

9.AE.25

9 : SILICATES (Germanates)
A : Nesosilicates
E : Nesosilicates with additional anions (O,OH,F,H2O); cations in tetrahedral [4] coordination
52.2.1.4

52 : NESOSILICATES Insular SiO4 Groups and O,OH,F,H2O
2 : Insular SiO4 Groups and O, OH, F, and H2O with cations in [4] and >[4] coordination
14.7.21

14 : Silicates not Containing Aluminum
7 : Silicates of Ba, Sr and Zn

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

Physical Properties of GerstmanniteHide

Sub-Adamantine, Vitreous, Silky
Transparency:
Translucent, Opaque
Comment:
silky when matted
Colour:
White to very pale pink.
Streak:
White
Hardness:
4½ on Mohs scale
Cleavage:
Distinct/Good
good on {010}
Density:
3.68(2) g/cm3 (Measured)    3.66 g/cm3 (Calculated)

Optical Data of GerstmanniteHide

Type:
Biaxial (-)
RI values:
nα = 1.655(2) nβ = 1.657(2) nγ = 1.678(2)
2V:
Measured: 50° to 60°, Calculated: 36°
Max. Birefringence:
δ = 0.023
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:
weak

Chemistry of GerstmanniteHide

Mindat Formula:
MnMgZn(SiO4)(OH)2
Element Weights:
Element% weight
O35.460 %
Zn24.150 %
Mn20.293 %
Si10.374 %
Mg8.978 %
H0.745 %

Calculated from ideal end-member formula.
O
Zn
Mn
Si
Mg
H
Common Impurities:
Fe,Na

Crystallography of GerstmanniteHide

Crystal System:
Orthorhombic
Class (H-M):
mmm(2/m2/m2/m) - Dipyramidal
Cell Parameters:
a = 8.185(7) Å, b = 18.65(2) Å, c = 6.256(6) Å
Ratio:
a:b:c = 0.439 : 1 : 0.335
Unit Cell V:
954.98 ų (Calculated from Unit Cell)
Z:
8
Comment:
Space Group: Bbcm

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0000554GerstmanniteMoore P B, Araki T (1977) Gerstmannite, a new zinc silicate mineral and a novel cubic close-packed oxide structure American Mineralogist 62 51-5919770293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
High-? alteration and/or metamorphism
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits

Type Occurrence of GerstmanniteHide

Place of Conservation of Type Material:
Harvard University, Cambridge, Massachusetts, 126484; National Museum of Natural History, Washington, D.C., USA, 135926, 137021.
Associated Minerals at Type Locality:

Synonyms of GerstmanniteHide

Other Language Names for GerstmanniteHide

Related Minerals - Strunz-mindat GroupingHide

9.AE.05BerylliteBe3(SiO4)(OH)2 · H2OOrth.
9.AE.10EuclaseBeAl(SiO4)(OH)Mon. 2/m : P21/b
9.AE.15SverigeiteNaMnMgSnBe2(SiO4)3(OH)Orth. mmm(2/m2/m2/m) : Imma
9.AE.20HodgkinsoniteMn2+Zn2(SiO4)(OH)2Mon. 2/m : P21/b
9.AE.30ClinohedriteCaZn(SiO4) · H2OMon. m : Bb
9.AE.35StringhamiteCaCu(SiO4) · H2OMon. 2/m : P21/b
9.AE.40Katoptrite(Mn2+,Mg)13(Al,Fe3+)4Sb5+2(SiO4)2O20Mon. 2/m : B2/m
9.AE.45YeatmaniteZn6Mn2+9Sb5+2(SiO4)4O12Tric. 1 : P1
9.AE.50SphaerobertranditeBe3(SiO4)(OH)2Mon. 2/m : P21/b

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 GerstmanniteHide

References for GerstmanniteHide

Localities for GerstmanniteHide

Showing 1 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)
 
  • New Jersey
    • Sussex County
      • Ogdensburg
        • Sterling Hill
Moore et al. (1977) +1 other reference
 
and/or  
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