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Rhodesite

A valid IMA mineral species - grandfathered
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About RhodesiteHide

09560760017271926233939.jpg
Cecil Rhodes
Formula:
KHCa2Si8O19 · 5H2O
Colour:
White
Lustre:
Silky
Hardness:
3 - 4
Specific Gravity:
2.27 - 2.36
Crystal System:
Orthorhombic
Member of:
Name:
Named after Cecil John Rhodes (1853-1902), British colonial statesman and financier of the Rhodes University, South Africa. He ran the British South Africa Company, which operated in a territory that became known as Rhodesia (named after him, now the countries of Zimbabwe and Zambia). He also founded the De Beers diamond company.
Related to fivegite. Not to be confused with Rhodizite.


Unique IdentifiersHide

Mindat ID:
3403
Long-form identifier:
mindat:1:1:3403:2

Similar NamesHide

Magnesio-riebeckiteA valid IMA mineral species - grandfathered◻Na2(Mg3Fe23+)(Si8O22)(OH)2
RhodiziteA valid IMA mineral species - grandfatheredKBe4Al4(B11Be)O28

IMA Classification of RhodesiteHide

Classification of RhodesiteHide

9.EB.05

9 : SILICATES (Germanates)
E : Phyllosilicates
B : Double nets with 4- and 6-membered rings
72.5.1.1

72 : PHYLLOSILICATES Two-Dimensional Infinite Sheets with Other Than Six-Membered Rings
5 : Two-Dimensional Infinite Sheets with Other Than Six-Membered Rings with corrugated and complex layers
14.6.7

14 : Silicates not Containing Aluminum
6 : Silicates of Ca with alkali or Mg or both

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

Pronunciation of RhodesiteHide

Pronunciation:
PlayRecorded byCountry
Jolyon RalphUnited Kingdom

Physical Properties of RhodesiteHide

Silky
Transparency:
Transparent, Translucent
Colour:
White
Hardness:
3 - 4 on Mohs scale
Cleavage:
Distinct/Good
Good on {100}
Density:
2.27 - 2.36 g/cm3 (Measured)    2.26 g/cm3 (Calculated)

Optical Data of RhodesiteHide

Type:
Biaxial (+)
RI values:
nα = 1.501 - 1.504 nβ = 1.506 - 1.508 nγ = 1.513 - 1.518
2V:
Calculated: 68.1°
Max. Birefringence:
δ = 0.012 - 0.014
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:
Low (negative)
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 strong

Chemistry of RhodesiteHide

Mindat Formula:
KHCa2Si8O19 · 5H2O
Element Weights:
Element% weight
O51.959 %
Si30.403 %
Ca10.846 %
K5.291 %
H1.500 %

Calculated from ideal end-member formula.
O
Si
Ca
K
H
Common Impurities:
Al,Fe,Mg,Na

Crystallography of RhodesiteHide

Crystal System:
Orthorhombic
Class (H-M):
mmm(2/m2/m2/m) - Dipyramidal
Cell Parameters:
a = 23.60(18) Å, b = 6.57(2) Å, c = 7.03(2) Å
Ratio:
a:b:c = 3.592 : 1 : 1.07
Unit Cell V:
1,090.02 ų (Calculated from Unit Cell)
Z:
2
Morphology:
Matted silky fibers, flattened rosettes, irregular segregations, crusts.
Comment:
Space Group: Pmam:

Crystal StructureHide

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IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0011015RhodesiteHesse K F, Liebau F, Merlino S (1992) Crystal structure of rhodesite, HK1-xNax+2yCa2-y(lB,3,22)(Si8O19)*(6-z)H2O, from three localities and its relation to other silicates with dreier double layers Zeitschrift fur Kristallographie 199 25-481992San Venanzo, Italy0293
0011014RhodesiteHesse K F, Liebau F, Merlino S (1992) Crystal structure of rhodesite, HK1-xNax+2yCa2-y(lB,3,22)(Si8O19)*(6-z)H2O, from three localities and its relation to other silicates with dreier double layers Zeitschrift fur Kristallographie 199 25-481992Trinity County, California, USA0293
0011013RhodesiteHesse K F, Liebau F, Merlino S (1992) Crystal structure of rhodesite, HK1-xNax+2yCa2-y{lB,3,2}[Si8O19]*(6-z)H2O, from three localities and its relation to other silicates with dreier double layers Zeitschrift fur Kristallographie 199 25-481992Zeilberg, Germany0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
6.548 Å(100)
4.386 Å(47)
5.901 Å(34)
6.302 Å(32)
5.032 Å(28)
2.864 Å(25)
2.762 Å(23)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 3a: Earth’s earliest Hadean crust>4.50
7 : Ultramafic igneous rocks
Stage 4b: Highly evolved igneous rocks>3.0
35 : Ultra-alkali and agpaitic igneous rocks
Geological Setting:
Kimberlite, altered silicic lavas

Type Occurrence of RhodesiteHide

Other Language Names for RhodesiteHide

Dutch:Rhodesiet
German:Rhodesit
Russian:Родзит
Spanish:Rhodesita

Relationship of Rhodesite to other SpeciesHide

Member of:
Other Members of Rhodesite Group:
Delhayelite(Na,K)10Ca5Al6Si32O80(Cl2,F2,SO4)3 · 18H2OOrth.
FivegiteK4Ca2[AlSi7O17(O2-xOHx)][(H2O)2-xOHx]ClOrth. mm2 : Pmn21
HydrodelhayeliteKCa2AlSi7O17(OH)2 · 6H2OOrth. mm2
MelansoniteNa◻KZrSi8O19 · 5H2OOrth. mmm(2/m2/m2/m) : Pmma
Monteregianite-(Y)(Na,K)6(Y,Ca)2Si16O38 · 10H2OMon. 2/m
NatromelansoniteNa3Zr[Si7AlO19] · 4H2OMon. 2/m : P21/m

Common AssociatesHide

Associations Based on Photo Data:
1 photo of Rhodesite associated with TridymiteSiO2
1 photo of Rhodesite associated with Fluorapophyllite-(K)KCa4(Si8O20)(F,OH) · 8H2O

Related Minerals - Strunz-mindat GroupingHide

9.EB.NatromelansoniteNa3Zr[Si7AlO19] · 4H2OMon. 2/m : P21/m
9.EB.05MelansoniteNa◻KZrSi8O19 · 5H2OOrth. mmm(2/m2/m2/m) : Pmma
9.EB.05MacdonalditeBaCa4Si16O36(OH)2 · 10H2OOrth.
9.EB.10HydrodelhayeliteKCa2AlSi7O17(OH)2 · 6H2OOrth. mm2
9.EB.10Delhayelite(Na,K)10Ca5Al6Si32O80(Cl2,F2,SO4)3 · 18H2OOrth.
9.EB.15Monteregianite-(Y)(Na,K)6(Y,Ca)2Si16O38 · 10H2OMon. 2/m
9.EB.20CarletoniteKNa4Ca4Si8O18(CO3)4(OH,F) · H2OTet. 4/mmm(4/m2/m2/m) : P4/mbm
9.EB.20FluorcarletoniteKNa4Ca4Si8O18(CO3)4F · H2OTet.
9.EB.25Günterblassite(K,Ca,Ba)2(Fe,Ca,Mg,Na)[(Si,Al)13O25(OH)4] · 7H2O · Orth. mm2 : Pmn21
9.EB.25Hillesheimite(K,Ca,Ba,◻)2(Mg,Fe,Ca,◻)2[(Si,Al )13O23(OH)6](OH) · 8H2OOrth. mmm(2/m2/m2/m) : Pmmn
9.EB.25UmbrianiteK7Na2Ca2[Al3Si10O29]F2Cl2 Orth. mmm(2/m2/m2/m) : Pmmn
9.EB.30FivegiteK4Ca2[AlSi7O17(O2-xOHx)][(H2O)2-xOHx]ClOrth. mm2 : Pmn21

RadioactivityHide

Radioactivity:
Element % Content Activity (Bq/kg) Radiation Type
Uranium (U) 0.0000% 0 α, β, γ
Thorium (Th) 0.0000% 0 α, β, γ
Potassium (K) 5.2906% 1,640 β, γ

For comparison:

  • Banana: ~15 Bq per fruit
  • Granite: 1,000–3,000 Bq/kg
  • EU exemption limit: 10,000 Bq/kg

Note: Risk is shown relative to daily recommended maximum exposure to non-background radiation of 1000 µSv/year. Note that natural background radiation averages around 2400 µSv/year so in reality these risks are probably extremely overstated! With infrequent handling and safe storage natural radioactive minerals do not usually pose much risk.

Interactive Simulator:

Note: The mass selector refers to the mass of radioactive mineral present, not the full specimen, also be aware that the matrix may also be radioactive, possibly more radioactive than this mineral!

Activity:

DistanceDose rateRisk
1 cm
10 cm
1 m

The external dose rate (D) from a radioactive mineral is estimated by summing the gamma radiation contributions from its Uranium, Thorium, and Potassium content, disregarding daughter-product which may have a significant effect in some cases (eg 'pitchblende'). This involves multiplying the activity (A, in Bq) of each element by its specific gamma ray constant (Γ), which accounts for its unique gamma emissions. The total unshielded dose at 1 cm is then scaled by the square of the distance (r, in cm) and multiplied by a shielding factor (μshield). This calculation provides a 'worst-case' or 'maximum risk' estimate because it assumes the sample is a point source and entirely neglects any self-shielding where radiation is absorbed within the mineral itself, meaning actual doses will typically be lower. The resulting dose rate (D) is expressed in microsieverts per hour (μSv/h).

D = ((AU × ΓU) + (ATh × ΓTh) + (AK × ΓK)) / r2 × μshield

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 RhodesiteHide

References for RhodesiteHide

Localities for RhodesiteHide

Showing 13 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.
Austria
 
  • Styria
    • Südoststeiermark District
      • Bad Gleichenberg
        • Wilhelmsdorf
Exel (1993) +1 other reference
      • Feldbach
        • Mühldorf bei Feldbach
Postl (1987) +2 other references
      • Klöch
Taucher (1989)
Germany
 
  • Bavaria
    • Lower Franconia
      • Haßberge District
        • Maroldsweisach
Jakob (1976) +2 other references
    • Upper Palatinate
      • Tirschenreuth District
        • Pechbrunn
Personal information of Erich Keck +1 other reference
  • Hesse
    • Darmstadt
      • Wetteraukreis
        • Ortenberg
  • Rhineland-Palatinate
    • Mayen-Koblenz
      • Vordereifel
        • Ettringen
Blaß et al. (1996)
Italy
 
  • Umbria
    • Terni Province
      • San Venanzo
Stoppa et al. (1997) +1 other reference
South Africa (TL)
 
  • Northern Cape
    • Frances Baard District Municipality
      • Sol Plaatje Local Municipality
        • Kimberley
          • KEM JV Mine (Kimberley Ekapa Mining Joint Venture mine; Kimberley Underground mine)
Mountain (1957) +1 other reference
Tanzania
 
  • Arusha region
    • Ngorongoro District
Tony Peterson Collection +1 other reference
Ukraine
 
Baranov et al. (2009)
USA
 
  • California
    • Fresno County
      • Big Creek-Rush Creek Mining District
Färber (n.d.)
    • Trinity County
      • Klamath Mountains
        • Trinity Mountains
          • Halls Gulch Mining District
            • Wildcat Peak
Sheppard et al. (1969) +3 other references
 
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