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Roeblingite

A valid IMA mineral species - grandfathered
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About RoeblingiteHide

04143770017271926394149.jpg
Washington Augustus Roebling
Formula:
Pb2Ca6Mn2+(Si3O9)2(SO4)2(OH)2 · 4H2O
Colour:
White, greyish white
Lustre:
Dull
Hardness:
3
Specific Gravity:
3.433
Crystal System:
Monoclinic
Name:
Named in 1897 by Samuel Lewis Penfield and Harry Ward Foote in honor of Colonel Washington A. Roebling (26 May 1837, Saxonburg, Pennsylvania, USA – 21 July 1926, Trenton, New Jersey, USA), founder of the Mineralogical Society of America, engineer, inventor of the diving bell, builder of the Brooklyn Bridge, and avid mineral collector, donated collection to Smithsonian.
This page provides mineralogical data about Roeblingite.


Unique IdentifiersHide

Mindat ID:
3436
Long-form identifier:
mindat:1:1:3436:0

IMA Classification of RoeblingiteHide

Approved, 'Grandfathered' (first described prior to 1959)
IMA Formula:
Pb2+2Ca6Mn2+(Si3O9)2(S6+O4)2(OH)2·4H2O
First published:
1897

Classification of RoeblingiteHide

9.CB.05

9 : SILICATES (Germanates)
C : Cyclosilicates
B : [Si3O9]6- 3-membered single rings, with insular complex anions
64.2.2.1

64 : CYCLOSILICATES Rings with Other Anions and Insular Silicate Groups
2 : Rings with Other Anions and Insular Silicate Groups: 3-membered rings with other anion groups
17.10.25

17 : Silicates Containing other Anions
10 : Silicates with sulphate, molybdate or tungstate

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

Physical Properties of RoeblingiteHide

Transparency:
Transparent, Opaque
Colour:
White, greyish white
Streak:
White
Hardness:
Cleavage:
Perfect
on {001}
Density:
3.433 g/cm3 (Measured)    3.44 g/cm3 (Calculated)

Optical Data of RoeblingiteHide

Type:
Biaxial (+)
RI values:
nα = 1.64 nβ = 1.64 nγ = 1.66
2V:
Measured: 61° (2), Calculated: 61°
Max. Birefringence:
δ = 0.020
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:
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:
relatively weak r < v

Chemistry of RoeblingiteHide

Mindat Formula:
Pb2Ca6Mn2+(Si3O9)2(SO4)2(OH)2 · 4H2O
Element Weights:
Element% weight
O34.959 %
Pb28.296 %
Ca16.420 %
Si11.506 %
S4.379 %
Mn3.751 %
H0.688 %

Calculated from ideal end-member formula.
O
Pb
Ca
Si
S
Mn
H
Common Impurities:
Sr,Na,K,C

Crystallography of RoeblingiteHide

Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
B2/m
Setting:
C2/m
Cell Parameters:
a = 13.208 Å, b = 8.287 Å, c = 13.089 Å
β = 106.65°
Ratio:
a:b:c = 1.594 : 1 : 1.579
Unit Cell V:
1,372.59 ų (Calculated from Unit Cell)
Z:
2
Morphology:
As dense, compact masses of tiny lathlike crystals.

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0000963RoeblingiteMoore P B, Shen J (1984) Roeblingite, Pb2Ca6(SO4)2(OH)2(H2O)4[Mn(Si3O9)2]: Its crystal structure and comments on the lone pair effect American Mineralogist 69 1173-117919840293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
3.15 Å(100)
4.20 Å(80)
3.04 Å(55)
2.102 Å(40)
6.47 Å(35)
6.29 Å(35)
2.947 Å(35)

Geological EnvironmentHide

Paragenetic Mode(s):
Geological Setting:
Metamorphosed manganese deposits.

Type Occurrence of RoeblingiteHide

General Appearance of Type Material:
Porcelanous
Place of Conservation of Type Material:
National Museum of Natural History, Washington, D.C., USA, R8824,124351.
The Natural History Museum, London, England, 1925,69.
Geological Setting of Type Material:
Highly altered (metasomatized) zone in a zinc-manganese-iron silicate-oxide orebody.
Associated Minerals at Type Locality:

Other Language Names for RoeblingiteHide

Common AssociatesHide

Associations Based on Photo Data:
23 photos of Roeblingite associated with HendricksiteKZn3(Si3Al)O10(OH)2
22 photos of Roeblingite associated with ClinohedriteCaZn(SiO4) · H2O
21 photos of Roeblingite associated with Ganophyllite(K,Na)xMn2+6(Si,Al)10O24(OH)4 · nH2O (x = 1-2; n = 7-11)
18 photos of Roeblingite associated with XonotliteCa6(Si6O17)(OH)2
11 photos of Roeblingite associated with Hancockite(CaPb)(AlAlFe3+)O[Si2O7][SiO4](OH)
8 photos of Roeblingite associated with WillemiteZn2SiO4
6 photos of Roeblingite associated with CharlesiteCa6(Al,Si)2(SO4)2[B(OH)4](OH,O)12 · 26H2O
5 photos of Roeblingite associated with PrehniteCa2Al2Si3O10(OH)2
3 photos of Roeblingite associated with PennantiteMn2+5Al(AlSi3O10)(OH)8
1 photo of Roeblingite associated with RhodoniteCaMn3Mn[Si5O15]

Related Minerals - Strunz-mindat GroupingHide

9.CB.10Diversilite-(Ce)Na2(Ba,K)6Fe2+Ce2Ti3(Si3O9)3(HSiO4)3(OH,H2O)9Trig. 3
9.CB.15Ilímaussite-(Ce)(Na,K)7-8(Ba,K)10Ce5(Nb,Ti)6(Si3O9)4(Si9O18)O6(O,OH)24Trig. 32 : R32

Fluorescence of RoeblingiteHide

Dull red (SW 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 RoeblingiteHide

References for RoeblingiteHide

Reference List:

Localities for RoeblingiteHide

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.
Sweden
 
  • Värmland County
    • Filipstad
      • Långban Ore District
Holtstam et al. (1999) +1 other reference
USA
 
  • New Jersey
    • Sussex County
      • Franklin
Palache (1935) +3 other references
FOMS Millsite Committee (1986)
Penfield et al. (1897) +2 other references
 
and/or  
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