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Ellingsenite

A valid IMA mineral species
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About EllingseniteHide

02627450017272471865336.jpg
Hans Vidar Ellingsen at Herrebøkasa
Formula:
Na5Ca6Si18O38(OH)13 · 6H2O
Colour:
Colorless, White
Lustre:
Vitreous, Silky
Hardness:
4
Specific Gravity:
2.32
Crystal System:
Triclinic
Name:
Named after the amateur mineralogist Dr. Ing. Hans Vidar Ellingsen (17 October 1930, Dønna, Nordland, Norway - 30 August 2014) from Oslo, Norway.
Structurally related to martinite and gyrolite.
Similar to kodamaite.

A F-bearing variety, possibly a new mineral, has been described by Blaß et al. (2020). SEM-EDS analyses gave (neglecting O): Na 11, Ca 17, Si 58, F 14 at.%. The PXRD pattern was affected by preferred orientation, but a shift of the first basal reflection to 15.10 Å was observed (type material has 15.50 Å).


Unique IdentifiersHide

Mindat ID:
39667
Long-form identifier:
mindat:1:1:39667:5

IMA Classification of EllingseniteHide

Approved
IMA Formula:
Na5Ca6Si18O38(OH)13·6H2O
Approval year:
2009
First published:
2011

Classification of EllingseniteHide

9.EE.80

9 : SILICATES (Germanates)
E : Phyllosilicates
E : Single tetrahedral nets of 6-membered rings connected by octahedral nets or octahedral bands

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

Physical Properties of EllingseniteHide

Vitreous, Silky
Transparency:
Transparent
Comment:
Silky in aggregates
Colour:
Colorless, White
Comment:
Colorless ( Separate crystals); white (aggregates)
Streak:
White
Hardness:
Tenacity:
Sectile
Cleavage:
Perfect
on (001)
Comment:
"Smooth" fracture.
Density:
2.32(5) g/cm3 (Measured)    2.383 g/cm3 (Calculated)
Comment:
Measured by float–sink method in methylene iodide. Dcalc is from powder data. Dcalc from single crystal data is 2.363.

Optical Data of EllingseniteHide

Type:
Biaxial (-)
RI values:
nα = 1.520(2) nβ = 1.534(2) nγ = 1.536
Max. Birefringence:
δ = 0.016
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:
None to Very Low
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.

No measured or calculated 2V is on file for this mineral, so the value used here (41°) is estimated from its recorded refractive indices and optic sign, not from a direct 2V measurement.
Dispersion:
None.
Optical Extinction:
X = c.

Chemistry of EllingseniteHide

Mindat Formula:
Na5Ca6Si18O38(OH)13 · 6H2O
Element Weights:
Element% weight
O50.718 %
Si28.115 %
Ca13.373 %
Na6.393 %
H1.401 %

Calculated from ideal end-member formula.
O
Si
Ca
Na
H

Crystallography of EllingseniteHide

Crystal System:
Triclinic
Class (H-M):
1 - Pinacoidal
Space Group:
P1
Cell Parameters:
a = 9.55(3) Å, b = 9.395(8) Å, c = 16.329(3) Å
α = 100.2(1)°, β = 94.9(2)°, γ = 117.8(2)°
Ratio:
a:b:c = 1.016 : 1 : 1.738
Unit Cell V:
1,251.52 ų (Calculated from Unit Cell)
Z:
1
Morphology:
Rhomb-like crystals, flattened on [001] and elongated on [100]. Dominate forms: pinacoidal {001} and {hk0}. The crystals forms commonly sheaf-like and radiating spherulite aggregates.
Twinning:
None observed

X-Ray Powder DiffractionHide

Powder Diffraction Data:
d-spacingIntensity
15.50 Å(100)
4.98 Å(14)
4.89 Å(14)
4.22 Å(16)
3.159 Å(30)
3.022 Å(33)
2.792 Å(24)
1.823 Å(30)

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 4b: Highly evolved igneous rocks>3.0
35 : Ultra-alkali and agpaitic igneous rocks
Stage 7: Great Oxidation Event<2.4
47a : [Near-surface hydration of prior minerals]
Geological Setting:
Hydrothermally altered phonolite .

Type Occurrence of EllingseniteHide

General Appearance of Type Material:
In vesicles in the phonolite. Rhomb-like crystals, usually arranged in sheaf-like and radiating aggregates.
Place of Conservation of Type Material:
Mineralogical Museum, St. Petersburg State University, Russia (1/19443).
Natural History Museum, Oslo University, Norway (42188).
Geological Setting of Type Material:
A hydrothermally altered phonolite of the Aris alkaline complex.
Associated Minerals at Type Locality:

Synonyms of EllingseniteHide

Other Language Names for EllingseniteHide

Common AssociatesHide

Associations Based on Photo Data:
54 photos of Ellingsenite associated with VilliaumiteNaF
38 photos of Ellingsenite associated with AegirineNaFe3+Si2O6
33 photos of Ellingsenite associated with TuperssuatsiaiteFe3+Fe3+2(Na◻)◻2Si8O20(OH)2(H2O)4 · 2H2O
5 photos of Ellingsenite associated with 'Unnamed (Fe-analogue of Zakharovite)'Na4Fe5Si10O24(OH)6 · 6H2O
3 photos of Ellingsenite associated with NatroliteNa2Al2Si3O10 · 2H2O
3 photos of Ellingsenite associated with AnalcimeNa(AlSi2O6) · H2O
2 photos of Ellingsenite associated with FluoriteCaF2
2 photos of Ellingsenite associated with Apophyllite GroupAB4[Si8O20]X · 8H2O
2 photos of Ellingsenite associated with MicroclineK(AlSi3O8)
2 photos of Ellingsenite associated with MakatiteNa2Si4O8(OH)2 · 4H2O

Related Minerals - Strunz-mindat GroupingHide

9.EE.CairncrossiteSr2Ca7-xNa2x(Si4O10)4(OH)2(H2O)15-xTric. 1 : P1
9.EE.05BementiteMn7Si6O15(OH)8Mon.
9.EE.07InnsbruckiteMn33(Si2O5)14(OH)38Mon. m : Bm
9.EE.10'Brokenhillite'Mn8Si6O15(OH)10Hex. 6mm : P63mc
9.EE.10Mcgillite(Mn,Fe)8Si6O15(OH)8Cl2Mon. 2/m : B2/m
9.EE.10FriedeliteMn2+8Si6O15(OH,Cl)10Mon. 2/m : B2/m
9.EE.10Pyrosmalite-(Mn)Mn2+8Si6O15(OH,Cl)10Trig. 3m(32/m) : P3m1
9.EE.10Pyrosmalite-(Fe)Fe2+8Si6O15(OH,Cl)10Trig. 3m(32/m) : P3m1
9.EE.15NeleniteMn2+16As3+3Si12O36(OH)17Trig. 3m(32/m) : R3m
9.EE.15SchalleriteMn2+16As3Si12O36(OH)17Trig. 3m : P3m1
9.EE.20Palygorskite◻Al2Mg22Si8O20(OH)2(H2O)4 · 4H2OMon. 2/m : B2/m
9.EE.20YofortieriteMn2+Mn2+2Mn2+22Si8O20(OH)2(H2O)4 · 4H2OMon. 2/m : B2/m
9.EE.20WindhoekiteFe3+(Fe3+1.670.33)Ca22Si8O20(OH)2(H2O)4(OH)2 · 6H2OMon. 2/m : B2/m
9.EE.20Windmountainite◻Fe3+2Mg22Si8O20(OH)2(H2O)4 · 4H2OMon. 2/m : B2/m
9.EE.20IkorskyiteKMn3+(Si4O10) · 3H2OMon. 2/m : P21/b
9.EE.20TuperssuatsiaiteFe3+Fe3+2(Na◻)◻2Si8O20(OH)2(H2O)4 · 2H2OMon. 2/m : B2/m
9.EE.20'Unnamed (Na-Ca-Fe-Silicate-Hydrate)'NaCa(Fe2+,Al,Mn)5[Si8O19(OH)](OH)7 · 5H2OTric. 1 : P1
9.EE.25SepioliteMg4(Si6O15)(OH)2 · 6H2OOrth. mmm(2/m2/m2/m) : Pnna
9.EE.25LoughliniteNa2Mg3Si6O16 · 8H2OOrth. mmm(2/m2/m2/m)
9.EE.25Falcondoite(Ni,Mg)4Si6O15(OH)2 · 6H2OOrth.
9.EE.25Kalifersite(K,Na)5Fe3+7Si20O50(OH)6 · 12H2OTric. 1 : P1
9.EE.30OrlymaniteCa4Mn3Si8O20(OH)6 · 2H2OHex.
9.EE.30TungusiteCa4Fe2Si6O15(OH)6Tric. 1 : P1
9.EE.30GyroliteNaCa16Si23AlO60(OH)8 · 14H2OTric. 1 : P1
9.EE.35Reyerite(Na,K)2Ca14(Si,Al)24O58(OH)8 · 6H2OTrig. 3 : P3
9.EE.35KodamaiteNa3(Ca5Na)Si16O36(OH)4F2 · (14-x)H2OTric. 1 : P1
9.EE.35Truscottite(Ca,Mn)14Si24O58(OH)8 · 2H2OTrig.
9.EE.40NatrosiliteNa2Si2O5Mon. 2/m : P21/b
9.EE.45MakatiteNa2Si4O8(OH)2 · 4H2OMon. 2/m : P21/b
9.EE.50VarennesiteNa8Mn2Si10O25(OH,Cl)2 · 12H2OOrth. mmm(2/m2/m2/m) : Cmcm
9.EE.55RaiteMn2+Mn2+2Na2(◻1.75Ti0.25)Si8O20(OH)2(H2O)4 · Na(H2O)6Orth. 222 : C222
9.EE.60IntersiliteNa6Mn2+Ti[Si10O24(OH)](OH)3 · 4H2OMon.
9.EE.65ZakharoviteNa4Mn5Si10O24(OH)6 · 6H2OTrig. 3m
9.EE.65ShafranovskiteNa3K2(Mn,Fe,Na)4[Si9(O,OH)27](OH)2 · nH2OTrig. 3m : P31c
9.EE.70ZeophylliteCa13Si10O28(OH)2F8 · 6H2OTrig. 3 : R3
9.EE.75Minehillite(K,Na)2-3Ca28Zn4Al4Si40O112(OH)16Hex.
9.EE.80Fedorite(Na,K)2-3(Ca4Na3)Si16O38(OH,F)2 · 3.5H2OTric. 1 : P1
9.EE.80Martinite(Na,◻,Ca)12Ca4(Si,S,B)14B2O38(OH,Cl)2F2 · 4H2OTric. 1 : P1
9.EE.85Lalondeite(Na,Ca)6(Ca,Na)3Si16O38(F,OH)2 · 3H2OTric. 1 : P1

Other InformationHide

Notes:
Insoluble in 1:1 HCl at room temperature.
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 EllingseniteHide

References for EllingseniteHide

Localities for EllingseniteHide

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.
Namibia (TL)
 
  • Khomas Region
    • Windhoek Rural
      • Aris
Yakovenchuk et al. (2011) +1 other reference
 
and/or  
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