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Hodgkinsonite

A valid IMA mineral species - grandfathered
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About HodgkinsoniteHide

Formula:
Mn2+Zn2(SiO4)(OH)2
Colour:
Bright pink or red to reddish brown and orange, pale pink, rarely yellow; black from tarnishing or inclusions.
Hardness:
4½ - 5
Specific Gravity:
4.06 - 4.08
Crystal System:
Monoclinic
Name:
Named in 1913 by Charles Palache and Waldemar Theodore Schaller in recognition of Harold Howe Hodgkinson [June 2, 1886 Toronto, Ontario, Canada - October 10, 1947 New Rochelle, New York, USA], assistant Underground Superintendent of the Franklin Mine and the person who brought the mineral to the attention of Charles Palache. In later life, Hodgkinson rose in business to be president of the Hodge and Hammond Company, dealers of construction equipment in the Bronx, New York.

Unique IdentifiersHide

Mindat ID:
1913
Long-form identifier:
mindat:1:1:1913:8

IMA Classification of HodgkinsoniteHide

Approved, 'Grandfathered' (first described prior to 1959)
IMA Formula:
Zn2+2Mn2+SiO4(OH)2

Classification of HodgkinsoniteHide

9.AE.20

9 : SILICATES (Germanates)
A : Nesosilicates
E : Nesosilicates with additional anions (O,OH,F,H2O); cations in tetrahedral [4] coordination
52.2.1.3

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
14.7.20

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

Physical Properties of HodgkinsoniteHide

Transparency:
Transparent, Translucent
Colour:
Bright pink or red to reddish brown and orange, pale pink, rarely yellow; black from tarnishing or inclusions.
Hardness:
4½ - 5 on Mohs scale
Cleavage:
Perfect
{011}
Density:
4.06 - 4.08 g/cm3 (Measured)    4.07 g/cm3 (Calculated)

Optical Data of HodgkinsoniteHide

Type:
Biaxial (-)
RI values:
nα = 1.720 - 1.724 nβ = 1.741 - 1.742 nγ = 1.746
2V:
Measured: 50° to 60°
Max. Birefringence:
δ = 0.022 - 0.026
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 moderate
Pleochroism:
Weak
Comments:
In shades of lavender and pale purple.

Chemistry of HodgkinsoniteHide

Mindat Formula:
Mn2+Zn2(SiO4)(OH)2
Element Weights:
Element% weight
Zn41.938 %
O30.788 %
Mn17.620 %
Si9.008 %
H0.647 %

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

Crystallography of HodgkinsoniteHide

Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
P21/b
Setting:
P21/a
Cell Parameters:
a = 11.761(2) Å, b = 5.316(2) Å, c = 8.171(2) Å
β = 95.25(8)°
Ratio:
a:b:c = 2.212 : 1 : 1.537
Unit Cell V:
508.72 ų (Calculated from Unit Cell)
Z:
4

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0015595HodgkinsoniteSolov'eva L P, Belov N V (1963) Crystal structure of hodgkinsonite Zn2Mn[SiO4](OH)2 Soviet Physics Doklady 8 867-8701963Franklin, New Jersey0293
0010606HodgkinsoniteRentzeperis P J (1963) The crystal structure of hodgkinsonite Zn2Mn[(OH)2|SiO4] Zeitschrift fur Kristallographie 119 117-1381963Franklin, New Jersey0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
2.864 Å(100)
2.957 Å(90)
1.547 Å(85)
2.567 Å(65)
1.412 Å(65)
2.115 Å(60)
1.594 Å(60)

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 HodgkinsoniteHide

Place of Conservation of Type Material:
Harvard University, Cambridge, Massachusetts, 89875, 89880, 89881; National Museum of Natural History, Washington, D.C., USA, 87231.
Associated Minerals at Type Locality:

Other Language Names for HodgkinsoniteHide

Common AssociatesHide

Associations Based on Photo Data:
39 photos of Hodgkinsonite associated with WillemiteZn2SiO4
38 photos of Hodgkinsonite associated with FrankliniteZn2+Fe3+2O4
37 photos of Hodgkinsonite associated with ZinciteZnO
34 photos of Hodgkinsonite associated with HetaeroliteZnMn2O4
14 photos of Hodgkinsonite associated with Chlorophoenicite(Mn,Mg)3Zn2(AsO4)(OH,O)6
12 photos of Hodgkinsonite associated with BaryteBaSO4
11 photos of Hodgkinsonite associated with Native CopperCu
7 photos of Hodgkinsonite associated with LennilenapeiteK4Mn2+48[Si64Al8]O164(OH)52 · nH2O
6 photos of Hodgkinsonite associated with FluoriteCaF2
6 photos of Hodgkinsonite associated with CalciteCaCO3

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.25GerstmanniteMnMgZn(SiO4)(OH)2Orth. mmm(2/m2/m2/m)
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

Fluorescence of HodgkinsoniteHide

weak pinkish red in LW UV.

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 HodgkinsoniteHide

References for HodgkinsoniteHide

Localities for HodgkinsoniteHide

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.
USA (TL)
 
  • New Jersey
    • Sussex County
      • Franklin
Palache et al. (1913) +3 other references
Palache (1935)
FOMS Millsite Committee (1986)
      • Ogdensburg
        • Sterling Hill
Cook (1973) +2 other references
 
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