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Simpsonite

A valid IMA mineral species - grandfathered
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About SimpsoniteHide

06049110017271926703045.jpg
Edward Sydney Simpson
Formula:
Al4Ta3O13(OH)
Colour:
Yellow, light brown or colourless, gray
Lustre:
Adamantine, Dull
Hardness:
7 - 7½
Specific Gravity:
6.35 (Calculated)
Crystal System:
Trigonal
Name:
Named in 1938 by Harry Bowley in honour of Edward Sydney Simpson (March 11, 1875, Woollahara, Western Australia, Australia - August 30, 1939, South Perth, Western Australia, Australia), government mineralogist and chemist of the Geological Survey of Western Australia. The Simpson Desert was also named for him.

Unique IdentifiersHide

Mindat ID:
3670
Long-form identifier:
mindat:1:1:3670:8

Similar NamesHide

IMA Classification of SimpsoniteHide

Approved, 'Grandfathered' (first described prior to 1959)
IMA Formula:
Al4Ta5+3O13(OH)
First published:
1939

Classification of SimpsoniteHide

4.DC.10

4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
D : Metal: Oxygen = 1:2 and similar
C : With medium-sized cations; sheets of edge-sharing octahedra
8.7.5.1

8 : MULTIPLE OXIDES CONTAINING NIOBIUM,TANTALUM OR TITANIUM
7 : Miscellaneous
18.1.19

18 : Niobates and Tantalates
1 : Niobates and tantalates containing neither rare earths nor U

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

Physical Properties of SimpsoniteHide

Adamantine, Dull
Transparency:
Translucent
Colour:
Yellow, light brown or colourless, gray
Streak:
White
Hardness:
7 - 7½ on Mohs scale
Tenacity:
Brittle
Cleavage:
None Observed
Density:
6.35 g/cm3 (Calculated)

Optical Data of SimpsoniteHide

Type:
Uniaxial (-)
RI values:
nω = 2.045 nε = 2.025
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.

Surface Relief:
Moderate

Chemistry of SimpsoniteHide

Mindat Formula:
Al4Ta3O13(OH)
Element Weights:
Element% weight
Ta61.985 %
O25.577 %
Al12.324 %
H0.115 %

Calculated from ideal end-member formula.

Crystallography of SimpsoniteHide

Crystal System:
Trigonal
Class (H-M):
3 - Pyramidal
Space Group:
P3
Cell Parameters:
a = 7.37 Å, c = 4.51 Å
Ratio:
a:c = 1 : 0.612
Unit Cell V:
212.15 ų (Calculated from Unit Cell)
Z:
1
Morphology:
Crystals tabular to short prismatic [0001].

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0005281SimpsoniteErcit T S, Cerny P, Hawthorne F C (1992) The crystal chemistry of simpsonite The Canadian Mineralogist 30 663-67119920293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Loading XRD data...
Data Set:
Data courtesy of RRUFF project at University of Arizona, used with permission.
Powder Diffraction Data:
d-spacingIntensity
1.651 Å(100)
2.859 Å(67)
3.69 Å(62)
2.131 Å(59)
1.395 Å(54)
2.417 Å(40)
2.609 Å(37)
Comments:
Alto do Giz pegmatite, Brazil. Data are from Ercit et al. (1992).

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 4b: Highly evolved igneous rocks>3.0
34 : Complex granite pegmatites

Type Occurrence of SimpsoniteHide

General Appearance of Type Material:
Poorly formed crystals approximating hexagonal prisms but showing only a few faces.
Place of Conservation of Type Material:
Western Australian Museum, Perth, numbers MDC1006, MDC1007.
The Natural History Museum, London, England, number 1938,122.
Geological Setting of Type Material:
Primary mineral in Ta-rich granite pegmatites.

Synonyms of SimpsoniteHide

Other Language Names for SimpsoniteHide

German:Simpsonit
Portuguese:Calogerasita
Spanish:Simpsonita

Common AssociatesHide

Associations Based on Photo Data:
19 photos of Simpsonite associated with Tantalite-(Mn)Mn2+Ta2O6
11 photos of Simpsonite associated with AlumotantiteAlTaO4
5 photos of Simpsonite associated with Rankamaite(Na,K)3(Ta,Nb,Al)11(O,OH)31
4 photos of Simpsonite associated with Hydroxykenomicrolite(◻,Na,Sb3+)2Ta2O6(OH,Cs)
3 photos of Simpsonite associated with CassiteriteSnO2
3 photos of Simpsonite associated with Tapiolite-(Fe)Fe2+Ta2O6
3 photos of Simpsonite associated with Microlite GroupA2-mTa2X6-wZ1-n
3 photos of Simpsonite associated with TitanowodginiteMn2+TiTa2O8
2 photos of Simpsonite associated with MicroclineK(AlSi3O8)
2 photos of Simpsonite associated with Tantalowodginite(Mn2+0.50.5)TaTa2O8

Related Minerals - Strunz-mindat GroupingHide

4.DC.05BahianiteAl5Sb3O14(OH)2Mon. 2/m : B2/m

Fluorescence of SimpsoniteHide

May fluoresce blue-white, 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 SimpsoniteHide

References for SimpsoniteHide

Reference List:

Localities for SimpsoniteHide

Showing 21 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.
Australia
 
  • Western Australia
    • Bridgetown-Greenbushes Shire
      • Greenbushes Mine
Jacobson et al. (2007)
    • East Pilbara Shire
von Knorring et al. (1963) +1 other reference
    • Yalgoo Shire
      • Dalgaranga Station
Jacobson et al. (2007) +2 other references
      • Meka Station
Jacobson et al. (2007) +2 other references
Brazil
 
  • Minas Gerais
    • Itinga
      • Monte Belo
Analysed (Reynaldo Contreira information) +1 other reference
  • Paraíba
    • Junco do Seridó
Pereira das Neves et al. (2018)
    • Equador
Lavinsky (n.d.) +5 other references
Canada
 
  • Manitoba
    • Lac-du-Bonnet area
      • Bernic Lake
www.davidkjoyceminerals.com +2 other references
DR Congo
 
  • Maniema
Uher et al. (2008)
  • North Kivu
    • Masisi Territory
      • Osso
        • Mumba
Safiannikoff et al. (1961) +2 other references
  • Tanganyika
Voloshin A.V. (1988)
Kazakhstan
 
  • East Kazakhstan Region
    • Ulan District
      • Asubulak ore field
        • Krasnokordon
Pekov (1998)
Pekov (1998)
Russia
 
  • Murmansk Oblast
Ponomareva et al. (2022)
Ponomareva et al. (2022)
Pavel M. Kartashov (n.d.) +3 other references
Zimbabwe
 
  • Mashonaland East
    • Mudzi District
Hornung. G. PhD thesis. Pegmatites of ...
von Knorring et al. (1963)
  • Masvingo
    • Bikita District
Černý et al. (2003)
McGregor (1946) +1 other reference
 
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