Erionite-K (original) (raw)
A valid IMA mineral species
About Erionite-KHide
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Formula:
(K2,Ca,Na2)2[Al4Si14O36] · 15H2O
Name:
Named in 1898 by Arthur Starr Eakle from the Greek εριον meaning wool in allusion to the "wooly" appearance of the type material. Erionite was first found at the Durkee Fire Opal Mine, Swayze Creek, Durkee, Baker Co., Oregon (Tschernich, 1992). In modern nomenclature, the original erionite was erionite-Na, but potassium was nearly equal to sodium. Levinson Rule suffix added in allusion to K dominant excangable cations.
A zeolite difficult to distinguish from offretite.
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:6916:4
9d13936f-7ed0-42e2-abf7-85dd5f2743b8
IMA Classification of Erionite-KHide
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IMA Formula:
K10[Si26Al10O72] · 30H2O
Classification of Erionite-KHide
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9.GD.20
9 : SILICATES (Germanates)
G : Tektosilicates with zeolitic H2O; zeolite family
D : Chains of 6-membered rings – tabular zeolites
Mineral SymbolsHide
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As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.
Please only use the official IMA–CNMNC symbol. Older variants are listed for historical use only.
Symbol | Source | Reference |
---|---|---|
Eri-K | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Eri | Whitney & Evans (2010) | Whitney, D.L. and Evans, B.W. (2010) Abbreviations for names of rock-forming minerals. American Mineralogist, 95, 185–187 doi:10.2138/am.2010.3371 |
Eri | Warr (2020) | Warr, L.N. (2020) Recommended abbreviations for the names of clay minerals and associated phases. Clay Minerals, 55, 261–264 doi:10.1180/clm.2020.30 |
Physical Properties of Erionite-KHide
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Optical Data of Erionite-KHide
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RI values:
_n_ω = 1.471 _n_ε = 1.474
δ = 0.003
Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
Chemistry of Erionite-KHide
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Mindat Formula:
(K2,Ca,Na2)2[Al4Si14O36] · 15H2O
Chemical AnalysisHide
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Empirical formulas:
Sample ID | Empirical Formula |
---|---|
1 | (K2.63Ca1.57Mg0.76Na0.13Ba0.01)[Si28.62Al7.35]O72·28.3H2O |
Crystallography of Erionite-KHide
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Class (H-M):
6/m m m _(_6/_m_2/_m_2/m ) - Dihexagonal Dipyramidal
Cell Parameters:
a = 13.227(1) Å, c = 15.075(3) Å
Unit Cell V:
2,284.08 ų (Calculated from Unit Cell)
Comment:
Cell parameters from Passaglia et al. 1998.
Crystal StructureHide
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ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
---|---|---|---|---|---|---|---|
0004973 | Erionite-K | Ballirano P, Andreozzi G B, Dogan M, Dogan A U (2009) Crystal structure and iron topochemistry of erionite-K from Rome, Oregon, U.S.A. American Mineralogist 94 1262-1270 | 2009 | Rome, Oregon, USA | 0 | 293 | |
0014439 | Erionite-K | Staples L W, Gard J A (1959) The fibrous zeolite erionite; its occurrence, unit cell, and structure Mineralogical Magazine 32 261-281 | 1959 | Durkee opal mine, Swayze Creek, Baker County, Oregon, USA | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder DiffractionHide
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Powder Diffraction Data:
d-spacing | Intensity |
---|---|
11.43 Å | (100) |
6.60 Å | (53) |
4.32 Å | (52) |
3.81 Å | (29) |
3.75 Å | (50) |
2.858 Å | (40) |
2.843 Å | (39) |
2.808 Å | (33) |
Comments:
Data from Eberly 1964; type material.
Geological EnvironmentHide
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Type Occurrence of Erionite-KHide
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Place of Conservation of Type Material:
No designated type material.
Other Language Names for Erionite-KHide
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Relationship of Erionite-K to other SpeciesHide
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Other Members of this group:
Erionite-Ca | (Ca,K2,Na2)2[Al4Si14O36] · 15H2O | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
---|---|---|
Erionite-Na | (Na2,K2,Ca)2[Al4Si14O36] · 15H2O | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
Common AssociatesHide
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Associated Minerals Based on Photo Data:
Related Minerals - Strunz-mindat GroupingHide
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9.GD.05 | Gmelinite-Ca | Ca2(Si8Al4)O24 · 11H2O | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
---|---|---|---|
9.GD.05 | Gmelinite-K | K4(Si8Al4O24) · 11H2O | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
9.GD.05 | Gmelinite-Na | Na4(Si8Al4)O24 · 11H2O | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
9.GD.10 | Willhendersonite | KCa[Al3Si3O12] · 5H2O | Tric. 1 : _P_1 |
9.GD.10 | Chabazite-Ca | (Ca,K2,Na2)2[Al2Si4O12]2 · 12H2O | Tric. 1 : _P_1 |
9.GD.10 | Chabazite-K | (K2,Ca,Na2,Sr,Mg)2[Al2Si4O12]2 · 12H2O | Trig. 3_m_ _(_32/m ) : R_3_m |
9.GD.10 | Chabazite-Na | (Na2,K2,Ca,Sr,Mg)2[Al2Si4O12]2 · 12H2O | Trig. 3_m_ : R_3_m |
9.GD.10 | Chabazite-Sr | Sr2[Al2Si4O12]2 · 12H2O | Trig. 3_m_ _(_32/m ) : R_3_m |
9.GD.10 | Chabazite-Mg | (Mg0.7K0.5Ca0.5Na0.1)[Al3Si9O24] · 10H2O | Trig. 3_m_ _(_32/m ) : R_3_m |
9.GD.15 | Lévyne-Ca | (Ca,Na2,K2)[Al2Si4O12] · 6H2O | Trig. 3_m_ _(_32/m ) : R_3_m |
9.GD.15 | Lévyne-Na | (Na2,Ca,K2)[Al2Si4O12] · 6H2O | Trig. 3_m_ _(_32/m ) : R_3_m |
9.GD.20 | Bellbergite | (K,Ba,Sr)2Sr2Ca2(Ca,Na)4[Al3Si3O12]6 · 30H2O | Hex. |
9.GD.20 | Erionite-Ca | (Ca,K2,Na2)2[Al4Si14O36] · 15H2O | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
9.GD.20 | Erionite-Na | (Na2,K2,Ca)2[Al4Si14O36] · 15H2O | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_63/m m c |
9.GD.25 | Offretite | KCaMg(Si13Al5)O36 · 15H2O | Hex. 6_m_2 : _P_6_m_2 |
9.GD.25 | Wenkite | (Ba,K)4(Ca,Na)6[(Si,Al)20O39(OH)2](SO4)3 · 0.5H2O | Hex. 6_m_2 : P_62_m |
9.GD.30 | Faujasite-Ca | (Ca,Na2,Mg)3.5[Al7Si17O48] · 32H2O | Iso. m_3_m _(_4/_m_32/m ) : F d_3_m |
9.GD.30 | Faujasite-Mg | (Mg,Na2,Ca)3.5[Al7Si17O48] · 32H2O | Iso. m_3_m _(_4/_m_32/m ) : F d_3_m |
9.GD.30 | Faujasite-Na | (Na2,Ca,Mg)3.5[Al7Si17O48] · 32H2O | Iso. m_3_m _(_4/_m_32/m ) : F d_3_m |
9.GD.35 | Maricopaite | Pb7Ca2(Si,Al)48O100 · 32H2O | Orth. |
9.GD.35 | Mordenite | (Na2,Ca,K2)4(Al8Si40)O96 · 28H2O | Orth. |
9.GD.40 | Dachiardite-K | K4(Si20Al4O48) · 13H2O | Mon. |
9.GD.40 | Dachiardite-Ca | (Ca,Na2,K2)5Al10Si38O96 · 25H2O | Mon. 2/m : _B_2/m |
9.GD.40 | Dachiardite-Na | (Na2,Ca,K2)5Al10Si38O96 · 25H2O | Mon. 2/m : _B_2/m |
9.GD.45 | Epistilbite | CaAl2Si6O16 · 5H2O | Mon. |
9.GD.50 | Ferrierite-K | (K,Na)5(Si31Al5)O72 · 18H2O | Orth. m m m _(_2/_m_2/_m_2/m ) : I m m m |
9.GD.50 | Ferrierite-Mg | [Mg2(K,Na)2Ca0.5](Si29Al7)O72 · 18H2O | Orth. m m m _(_2/_m_2/_m_2/m ) : P n n m |
9.GD.50 | Ferrierite-Na | (Na,K)5(Si31Al5)O72 · 18H2O | Mon. 2/m |
9.GD.50 | Ferrierite-NH4 | (NH4,Mg0.5)5(Al5Si31O72) · 22H2O | Orth. m m m _(_2/_m_2/_m_2/m ) : I m m m |
9.GD.55 | Bikitaite | LiAlSi2O6 · H2O | Tric. 1 : _P_1 |
Other InformationHide
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Health Risks:
Carcinogenic upon inhalation of its dust, due to its fibrous structure (Ref.: IARC Monography 42:225-239, 1987)
Internet Links for Erionite-KHide
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References for Erionite-KHide
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Reference List:
Gualtieri, A., Artioli, G., Passaglia, E., Bigi, S., Viani, A., Hanson, J. C. (1998) Crystal structure-crystal chemistry relationships in the zeolites erionite and offretite. American Mineralogist, 83 (5) 590-606 doi:10.2138/am-1998-5-619
Giacobbe, Carlotta, Moliterni, Anna, Di Giuseppe, Dario, Malferrari, Daniele, Wright, Jonathan P., Mattioli, Michele, Ranieri, Simona, Giannini, Cinzia, Fornasini, Laura, Mugnaioli, Enrico, Ballirano, Paolo, Gualtieri, Alessandro F. (2023) The crystal structure of the killer fibre erionite from Tuzköy (Cappadocia, Turkey) IUCrJ, 10 (4) 397-410 doi:10.1107/s2052252523003500
Localities for Erionite-KHide
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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.
Locality ListHide
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- 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.