Edingtonite (original) (raw)
A valid IMA mineral species - grandfathered
About EdingtoniteHide
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Formula:
Ba[Al2Si3O10] · 4H2O
Colour:
Colorless to white
Lustre:
Vitreous, Sub-Vitreous
Specific Gravity:
2.694 - 2.71
Crystal System:
Orthorhombic
Name:
Named in 1825 by Wilelm K. Haidinger and Edward Turner in honor of Scottish industrial chemist and mineral collector Thomas Edington [c. 18 Jul 1783 Cramond, Midlothian, Scotland - May 1841 Glasgow, Scotland].
Zeolite Group. Edingtonite Subgroup.
Most edingtonites are orthorhombic (space group _P_212121), while some are tetragonal (space group P_-421_m) and called 'tetraedingtonite'. Orthorhombic edingtonites have (Si,Al) order, while tetragonal edingtonites are characterised by (Si,Al) disorder (symmetry increase due to disorder).
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:1353:2
f428ac69-0768-475c-8a43-c66eb624cab4
IMA Classification of EdingtoniteHide
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Approved, 'Grandfathered' (first described prior to 1959)
IMA Formula:
Ba(Si3Al2)O10 · 4H2O
Type description reference:
Classification of EdingtoniteHide
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9.GA.15
9 : SILICATES (Germanates)
G : Tektosilicates with zeolitic H2O; zeolite family
A : Zeolites with T5O10 Units – The Fibrous Zeolites
77.1.5.6
77 : TECTOSILICATES Zeolites
1 : Zeolite group - True zeolites
16.12.7
16 : Silicates Containing Aluminum and other Metals
12 : Aluminosilicates of Sr, Ba and Zn
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.
Symbol | Source | Reference |
---|---|---|
Edi | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Pronunciation of EdingtoniteHide
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Pronunciation:
Play | Recorded by | Country |
---|---|---|
Sorry, your browser doesn't support HTML5 audio. | Jolyon Ralph | United Kingdom |
Physical Properties of EdingtoniteHide
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Transparency:
Transparent, Translucent
Colour:
Colorless to white
Density:
2.694 - 2.71 g/cm3 (Measured)
Optical Data of EdingtoniteHide
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RI values:
_n_α = 1.538 _n_β = 1.549 _n_γ = 1.554
δ = 0.016
Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
Dispersion:
r < v moderate
Chemistry of EdingtoniteHide
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Mindat Formula:
Ba[Al2Si3O10] · 4H2O
Crystallography of EdingtoniteHide
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Crystal System:
Orthorhombic
Class (H-M):
222 - Disphenoidal
Cell Parameters:
a = 9.550(10) Å, b = 9.665(10) Å, c = 6.523(5) Å
Ratio:
a:b:c = 0.988 : 1 : 0.675
Unit Cell V:
602.08 ų (Calculated from Unit Cell)
Comment:
Mazzi et al. (1984) concluded "that two types of edingtonite occur, "orthorhombic edingtonite" and "tetragonal edingtonite"." Space groups given are P212121 and P-421m (with Al-Si disorder), respectively. Data given here are for the orthorhombic variant.
Crystal StructureHide
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ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
---|---|---|---|---|---|---|---|
0003529 | Edingtonite | Gatta G D, Ballaran T B, Comodi P, Zanazzi P F (2004) Isothermal equation of state and compressional behavior of tetragonal edingtonite American Mineralogist 89 633-639 | 2004 | 0.0001 | 293 | ||
0003530 | Edingtonite | Gatta G D, Ballaran T B, Comodi P, Zanazzi P F (2004) Isothermal equation of state and compressional behavior of tetragonal edingtonite American Mineralogist 89 633-639 | 2004 | 0.0001 | 293 | ||
0003531 | Edingtonite | Gatta G D, Ballaran T B, Comodi P, Zanazzi P F (2004) Isothermal equation of state and compressional behavior of tetragonal edingtonite American Mineralogist 89 633-639 | 2004 | 2.285 | 293 | ||
0003532 | Edingtonite | Gatta G D, Ballaran T B, Comodi P, Zanazzi P F (2004) Isothermal equation of state and compressional behavior of tetragonal edingtonite American Mineralogist 89 633-639 | 2004 | 4.611 | 293 | ||
0006714 | Edingtonite | Stahl K, Hanson J C (1998) An in situ study of the edingtonite dehydration process from X-ray synchrotron powder diffraction European Journal of Mineralogy 10 221-228 | 1998 | 0 | 293 | ||
0006715 | Edingtonite | Stahl K, Hanson J C (1998) An in situ study of the edingtonite dehydration process from X-ray synchrotron powder diffraction European Journal of Mineralogy 10 221-228 | 1998 | 0 | 293 | ||
0006716 | Edingtonite | Stahl K, Hanson J C (1998) An in situ study of the edingtonite dehydration process from X-ray synchrotron powder diffraction European Journal of Mineralogy 10 221-228 | 1998 | 0 | 293 | ||
0006717 | Edingtonite | Stahl K, Hanson J C (1998) An in situ study of the edingtonite dehydration process from X-ray synchrotron powder diffraction European Journal of Mineralogy 10 221-228 | 1998 | 0 | 293 | ||
0017959 | Edingtonite | Taylor W (1935) An X-ray examination of substituted Edingtonites. _cod_database_code 1011059 Mineralogical Magazine 24 208-240 | 1935 | 0 | 293 | ||
0014790 | Edingtonite | Mazzi F, Galli E, Gottardi G (1984) Crystal structure refinement of two tetragonal edingtonites Neues Jahrbuch fur Mineralogie, Monatshefte 1984 373-382 | 1984 | Ice River, British Columbia, Canada | 0 | 293 | |
0014791 | Edingtonite | Mazzi F, Galli E, Gottardi G (1984) Crystal structure refinement of two tetragonal edingtonites Neues Jahrbuch fur Mineralogie, Monatshefte 1984 373-382 | 1984 | Old Kilpatrick, Dumbartonshire, Scotland | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder DiffractionHide
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Radiation - Copper Kα
Data Set:
Data courtesy of RRUFF project at University of Arizona, used with permission.
Powder Diffraction Data:
d-spacing | Intensity |
---|---|
3.576 Å | (100) |
6.51 Å | (80) |
2.741 Å | (75) |
5.38 Å | (60) |
4.79 Å | (50) |
4.69 Å | (50) |
2.589 Å | (45) |
Geological EnvironmentHide
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Type Occurrence of EdingtoniteHide
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Geological Setting of Type Material:
Found on Lord Blantyre's Estate, West Kilpatrick, Dumbartonshire, near Glasgow, Scottland.
Associated Minerals at Type Locality:
Reference:
Haidinger, W.K., Turner, E. (1825) Description of edingtonite, a new mineral species. The Edinburgh Journal of Science: 3: 316-320.
Synonyms of EdingtoniteHide
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Other Language Names for EdingtoniteHide
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Relationship of Edingtonite to other SpeciesHide
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Other Members of this group:
Alflarsenite | NaCa2Be3Si4O13(OH) · 2H2O | Mon. 2 : _P_21 |
---|---|---|
Amicite | K2Na2Al4Si4O16 · 5H2O | Mon. 2 |
Ammonioleucite | (NH4)(AlSi2O6) | Tet. 4/m : _I_41/a |
Analcime | Na(AlSi2O6) · H2O | Tric. 1 : _P_1 |
Bellbergite | (K,Ba,Sr)2Sr2Ca2(Ca,Na)4[Al3Si3O12]6 · 30H2O | Hex. |
Bikitaite | LiAlSi2O6 · H2O | Tric. 1 : _P_1 |
Boggsite | Ca8Na3(Si,Al)96O192 · 70H2O | Orth. m m m _(_2/_m_2/_m_2/m ) : I m m a |
Brewsterite Subgroup | Zeolite Group. | |
Chabazite-Levyne Subgroup | M[Al2Si4O12] · 6H2O | |
Chiavennite | CaMnBe2Si5O13(OH)2 · 2H2O | Mon. 2/m : _P_21/b |
Clinoptilolite Subgroup | M3-6(Si30Al6)O72 · 20H2O | |
Cowlesite | CaAl2Si3O10 · 6H2O | Orth. m m m _(_2/_m_2/_m_2/m ) |
Dachiardite Subgroup | Zeolite Group. | |
Direnzoite | NaK6MgCa2(Al13Si47O120) · 36H2O | Orth. m m m _(_2/_m_2/_m_2/m ) : P m m n |
Epistilbite | CaAl2Si6O16 · 5H2O | Mon. |
Erionite Subgroup | M2[Al4Si14O36] · 15H2O | |
Faujasite Subgroup | M3.5[Al7Si17O48] · 32H2O | |
Ferrierite Subgroup | Zeolite Group. | |
Ferrochiavennite | Ca1-2Fe[(Si,Al,Be)5Be2O13(OH)2] · 2H2O | Mon. 2/m : _P_21/b |
Flörkeite | (K3Ca2Na)[Al8Si8O32] · 12H2O | Tric. 1 : _P_1 |
Garronite Subgroup | ||
Gaultite | Na4Zn2Si7O18 · 5H2O | Orth. m _m_2 : F d _d_2 |
Gismondine Subgroup | Zeolite Group. | |
Gmelinite Subgroup | In 1997, gmelinite was split into Gmelinite-Ca, Gmelinite-Na and Gmelinite-K. | |
Gobbinsite | Na5(Si11Al5)O32 · 11H2O | Orth. m m m _(_2/_m_2/_m_2/m ) : P n m a |
Goosecreekite | Ca[Al2Si6O16] · 5H2O | Mon. 2 : _P_21 |
Gottardiite | Na3Mg3Ca5Al19Si117O272 · 93H2O | Orth. m m m _(_2/_m_2/_m_2/m ) : C m c a |
Heulandite Subgroup | (Na/Ca/K)5-6[Al8-9 Si27-28 O72] · nH2O | |
Hsianghualite | Ca3Li2(Be3Si3O12)F2 | Iso. 432 : _I_4132 |
Kirchhoffite | Cs(BSi2O6) | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _I_41/a c d |
Laumontite | CaAl2Si4O12 · 4H2O | Mon. 2/m : _B_2/m |
Loomisite | Ba[Be2P2O8] · H2O | Mon. m |
Lovdarite | K2Na6Be4Si14O36 · 9H2O | Orth. m _m_2 |
Maricopaite | Pb7Ca2(Si,Al)48O100 · 32H2O | Orth. |
Martinandresite | Ba2(Al4Si12O32) · 10H2O | Orth. m m m _(_2/_m_2/_m_2/m ) : P m m n |
Mazzite Subgroup | Zeolite Group. | |
Merlinoite | (K,Na)5(Ca,Ba)2Al9Si23O64 · 23H2O | Orth. m m m _(_2/_m_2/_m_2/m ) : I m m m |
Montesommaite | (K,Na)9Al9Si23O64 · 10H2O | Orth. m _m_2 : F d _d_2 |
Mordenite | (Na2,Ca,K2)4(Al8Si40)O96 · 28H2O | Orth. |
Mutinaite | Na3Ca4Si85Al11O192 · 60H2O | Orth. m m m _(_2/_m_2/_m_2/m ) : P n m a |
Nabesite | Na2BeSi4O10 · 4H2O | Orth. 222 : _P_212121 |
Natrolite Subgroup | A subgroup of the Zeolite Group. | |
Offretite | KCaMg(Si13Al5)O36 · 15H2O | Hex. 6_m_2 : _P_6_m_2 |
Pahasapaite | Li8(Ca,Li,K)10.5Be24(PO4)24 · 38H2O | Iso. 23 : _I_23 |
Parthéite | Ca2(Si4Al4) O15 (OH)2 · 4H2O | Mon. 2/m : _B_2/b |
Paulingite Subgroup | Paulingite was originally described in 1960. | |
Perlialite | K9Na(Ca,Sr)[Al2Si4O12]6 · 15H2O | Hex. 6/m m m _(_6/_m_2/_m_2/m ) : _P_6/m m m |
Phillipsite Subgroup | Zeolite Group. | |
Pollucite | (Cs,Na)2(Al2Si4O12) · 2H2O | Iso. m_3_m _(_4/_m_32/m ) : I a_3_d |
Roggianite | Ca2Be(OH)2Al2Si4O13 · 2.5H2O | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _I_4/m c m |
Stilbite Subgroup | M6-7[Al8-9Si27-28O72] · nH2O | |
Terranovaite | (Na,Ca)8(Si68Al12)O160 · 29H2O | Orth. |
Thomsonite Subgroup | The large majority of "thomsonite" is thomsonite-Ca. | |
Tschernichite | (Ca,Na2)[Al2Si4O12] · 4-8H2O | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _P_4/m m m |
Tschörtnerite | Ca4(Ca,Sr,K,Ba)3Cu3[Al3Si3O12]4(OH)8 · nH2O | Iso. m_3_m _(_4/_m_32/m ) : F m_3_m |
UM1996-38-SiO:AlCaHNa | Na-Ca-Al-Si-O-H | |
UM1999-33-SiO:AlHKNa | K7Na5Al12Si20O64 · 24H2O | |
UM2002-40-SiO:AlCaHKMgNa | (Mg,Ca,Na,K)7.5(Al12.8Si51.2)O128 · 65H2O | Tet. 422 : _P_4122 |
Unnamed (Ca analogue of Merlinoite) | (Ca,K,Na)5(Ca,Ba)2Al9Si23O64 · 23H2O ? | |
Wairakite | Ca(Al2Si4O12) · 2H2O | Mon. 2/m : _B_2/m |
Weinebeneite | CaBe3(PO4)2(OH)2 · 4H2O | Mon. m : B b |
Wenkite | (Ba,K)4(Ca,Na)6[(Si,Al)20O39(OH)2](SO4)3 · 0.5H2O | Hex. 6_m_2 : P_62_m |
Willhendersonite | KCa[Al3Si3O12] · 5H2O | Tric. 1 : _P_1 |
Yugawaralite | CaAl2Si6O16 · 4H2O | Mon. m : P b |
Structurally related to group(s):
Common AssociatesHide
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Associated Minerals Based on Photo Data:
Related Minerals - Strunz-mindat GroupingHide
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Other InformationHide
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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 EdingtoniteHide
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References for EdingtoniteHide
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Reference List:
Dunn, Pete J., Ferraiolo, James A., Fleischer, Michael, Gobel, Volker, Grice, Joel D., Langley, Richard H., Shigley, James E., Vanko, David A., Zilczer, Janet A. (1985) New mineral names. American Mineralogist, 70 (11-12) 1329-1335
Coombs, Douglas S., Alberti, Alberto, Armbruster, Thomas, Artioli, Gilberto, Colella, Carmine, Galli, Ermanno, Grice, Joel D., Liebau, Friedrich, Mandarino, Joseph A., Minato, Hideo, Nickel, Ernest H., Passaglia, Elio, Peacor, Donald R., Quartieri, Simona, Rinaldi, Romano, Ross, Malcolm I., Sheppard, Richard A., Tillmanns, Ekkehart, Vezzalini, Giovanna (1997) Recommended nomenclature for zeolite minerals; report of the Subcommittee on Zeolites of the International Mineralogical Association, Commission on New Minerals and Mineral Names. The Canadian Mineralogist, 35 (6) 1571-1606
Localities for EdingtoniteHide
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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.