Leucite
About Leucite
The mineral is usually included as a feldspathoid by petrologists, as it is a common primary rock-forming mineral in some high-potassium rocks but, despite being anhydrous, structurally it also has a topological relation to zeolites, especially analcime, and thus is typically included in that family also.
Visit gemdat.org for gemological information about Leucite.Unique Identifiers
Similar Names
| Leesite | A valid IMA mineral species | K(H2O)2[(UO2)4O2(OH)5] · 3H2O |
IMA Classification of Leucite
Classification of Leucite
9 : SILICATES (Germanates)
G : Tektosilicates with zeolitic H2O; zeolite family
B : Chains of single connected 4-membered rings
76 : TECTOSILICATES Al-Si Framework
2 : Al-Si Framework Feldspathoids and related species
16 : Silicates Containing Aluminum and other Metals
3 : Aluminosilicates of K
Mineral Symbols
Please only use the official IMA–CNMNC symbol. Older variants are listed for historical use only.
| Symbol | Source | Reference for Standard |
|---|---|---|
| Lct | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
| Lct | Kretz (1983) | Kretz, R. (1983) Symbols of rock-forming minerals. American Mineralogist, 68, 277–279. |
| Lct | Siivolam & Schmid (2007) | Siivolam, J. and Schmid, R. (2007) Recommendations by the IUGS Subcommission on the Systematics of Metamorphic Rocks: List of mineral abbreviations. Web-version 01.02.07. IUGS Commission on the Systematics in Petrology. download |
| Lct | 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 |
| Lct | The Canadian Mineralogist (2019) | The Canadian Mineralogist (2019) The Canadian Mineralogist list of symbols for rock- and ore-forming minerals (December 30, 2019). download |
Physical Properties of Leucite
Very poor om {110}
Optical Data of Leucite
Based on recorded range of RI values above.
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.
Relative to Canada balsam mounting medium (n ≈ 1.537).
For a genuinely uniaxial mineral viewed this way, that cross stays perfectly stationary if you rotate the stage - unlike a biaxial mineral, where it splits apart on rotation. That invariance is itself the standard diagnostic test for telling uniaxial and biaxial minerals apart at the microscope.
Chemistry of Leucite
Age distribution
| Sample ID | Recorded age | Geologic Time | Dating method |
|---|---|---|---|
| 1 | 0.056 ± 0.005 Ma | Pleistocene | K-Ar |
| 2 | 0.67 to 0.26 Ma | Pleistocene | |
| 3 | 0.79 ± 0.09 Ma | Pleistocene | K-Ar |
| 4 | 16.47 ± 1.22 Ma | Miocene | Ar-Ar of olivine-bearing leucite foidite |
| 5 | 30.8 ± 0.6 Ma | Oligocene | K-Ar |
| 6 | 51.8 ± 2.0 to 49.1 ± 2.0 Ma | Eocene |
Crystallography of Leucite
Crystallographic forms of Leucite
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Crystal Structure
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| ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
|---|---|---|---|---|---|---|---|
| 0004674 | Leucite | Gatta G D, Rotiroti N, Ballaran T B, Pavese A (2008) Leucite at high pressure: Elastic behavior, phase stability, and petrological implications American Mineralogist 93 1588-1596 | ![]() | 2008 | Sabatini volcanic district, Lazium, Italy | 0.0001 | 293 |
| 0004673 | Leucite | Gatta G D, Rotiroti N, Ballaran T B, Pavese A (2008) Leucite at high pressure: Elastic behavior, phase stability, and petrological implications American Mineralogist 93 1588-1596 | ![]() | 2008 | Sabatini volcanic district, Lazium, Italy | 0.0001 | 293 |
| 0010665 | Leucite | Peacor D R (1968) A high temperature single crystal diffractometer study of leucite, (K,Na)AlSi2O6 that reproduced the reported bond lengths and thermal ellipsoid axes. Zeitschrift fur Kristallographie 127 213-224 | ![]() | 1968 | Vesuvius, Italy | 0 | 293 |
| 0004675 | Leucite | Gatta G D, Rotiroti N, Ballaran T B, Pavese A (2008) Leucite at high pressure: Elastic behavior, phase stability, and petrological implications American Mineralogist 93 1588-1596 | ![]() | 2008 | Sabatini volcanic district, Lazium, Italy | 0.38 | 293 |
| 0004676 | Leucite | Gatta G D, Rotiroti N, Ballaran T B, Pavese A (2008) Leucite at high pressure: Elastic behavior, phase stability, and petrological implications American Mineralogist 93 1588-1596 | ![]() | 2008 | Sabatini volcanic district, Lazium, Italy | 1.2 | 293 |
| 0004677 | Leucite | Gatta G D, Rotiroti N, Ballaran T B, Pavese A (2008) Leucite at high pressure: Elastic behavior, phase stability, and petrological implications American Mineralogist 93 1588-1596 | ![]() | 2008 | Sabatini volcanic district, Lazium, Italy | 1.77 | 293 |
| 0001854 | Leucite | Palmer D C, Dove M T, Ibberson R M, Powell B M (1997) Structural behavior, crystal chemistry and phase transitions in substituted leucites: High-resolution neutron powder diffraction studies American Mineralogist 82 16-29 | ![]() | 1997 | 0 | 298 | |
| 0001853 | Leucite | Palmer D C, Dove M T, Ibberson R M, Powell B M (1997) Structural behavior, crystal chemistry and phase transitions in substituted leucites: High-resolution neutron powder diffraction studies American Mineralogist 82 16-29 | ![]() | 1997 | 0 | 298 | |
| 0001852 | Leucite | Palmer D C, Dove M T, Ibberson R M, Powell B M (1997) Structural behavior, crystal chemistry and phase transitions in substituted leucites: High-resolution neutron powder diffraction studies American Mineralogist 82 16-29 | ![]() | 1997 | 0 | 298 | |
| 0001851 | Leucite | Palmer D C, Dove M T, Ibberson R M, Powell B M (1997) Structural behavior, crystal chemistry and phase transitions in substituted leucites: High-resolution neutron powder diffraction studies American Mineralogist 82 16-29 | ![]() | 1997 | 0 | 298 | |
| 0001558 | Leucite | Dove M T, Cool T, Palmer D C, Putnis A, Salje E K H, Winkler B (1993) On the role of Al-Si ordering in the cubic-tetragonal phase transition of leucite Sample is Order model 2 American Mineralogist 78 486-492 | ![]() | 1993 | 0 | 293 | |
| 0001557 | Leucite | Dove M T, Cool T, Palmer D C, Putnis A, Salje E K H, Winkler B (1993) On the role of Al-Si ordering in the cubic-tetragonal phase transition of leucite Sample is Order model 1 American Mineralogist 78 486-492 | ![]() | 1993 | 0 | 293 | |
| 0001556 | Leucite | Dove M T, Cool T, Palmer D C, Putnis A, Salje E K H, Winkler B (1993) On the role of Al-Si ordering in the cubic-tetragonal phase transition of leucite Sample is Disordered American Mineralogist 78 486-492 | ![]() | 1993 | 0 | 293 | |
| 0000496 | Leucite | Mazzi F, Galli E, Gottardi G (1976) The crystal structure of tetragonal leucite American Mineralogist 61 108-115 | ![]() | 1976 | 0 | 293 | |
| 0017982 | Leucite | Wyart M (1940) Etude cristallographique d'une leucite artificielle. Structure atomique et symetrie du mineral _cod_database_code 1011086 Bulletin de la Societe Francaise de Mineralogie 63 5-17 | 1940 | 0 | 293 | ||
| 0017354 | Leucite | Wyart M (1940) Etude cristallographique d'une leucite artificielle. Structure atomique et symetrie du mineral _cod_database_code 1010431 Bulletin de la Societe Francaise de Mineralogie 63 5-17 | 1940 | 0 | 293 |
X-Ray Powder Diffraction
| d-spacing | Intensity |
|---|---|
| 3.266 Å | (100) |
| 3.438 Å | (85) |
| 5.39 Å | (80) |
| 2.918 Å | (70) |
| 2.842 Å | (70) |
| 2.366 Å | (65) |
| 2.808 Å | (55) |
Geological Environment
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Stage 3a: Earth’s earliest Hadean crust | >4.50 |
| 8 : Mafic igneous rocks | |
| 9 : Lava/xenolith minerals (hornfels, sanidinite facies) | |
| Stage 4b: Highly evolved igneous rocks | >3.0 |
| 35 : Ultra-alkali and agpaitic igneous rocks | |
| Stage 10a: Neoproterozoic oxygenation/terrestrial biosphere | <0.6 |
| 50 : Coal and/or oil shale minerals | <0.36 |
| Stage 10b: Anthropogenic minerals | <10 Ka |
| 54 : Coal and other mine fire minerals (see also #51 and #56) |
Type Occurrence of Leucite
Synonyms of Leucite
Other Language Names for Leucite
Relationship of Leucite to other Species
| Alflarsenite | NaCa2Be3Si4O13(OH) · 2H2O | Mon. 2 : P21 |
| Amicite | K2Na2Al4Si4O16 · 5H2O | Mon. 2 |
| Ammonioleucite | (NH4)(AlSi2O6) | Tet. 4/m : I41/a |
| Analcime | Na(AlSi2O6) · H2O | Tric. 1 : P1 |
| Arzamastsevite | K6Al5Si6O20(OH)4Cl | Tet. 42m : I42m |
| Bellbergite | (K,Ba,Sr)2Sr2Ca2(Ca,Na)4[Al3Si3O12]6 · 30H2O | Hex. |
| Bikitaite | LiAlSi2O6 · H2O | Tric. 1 : P1 |
| Boggsite | Ca8Na3(Si,Al)96O192 · 70H2O | Orth. mmm(2/m2/m2/m) : Imma |
| Brewsterite Subgroup | Zeolite Group. | |
| Chabazite-Levyne Subgroup | M[Al2Si4O12] · 6H2O | |
| Chiavennite | CaMnBe2Si5O13(OH)2 · 2H2O | Mon. 2/m : P21/b |
| Clinoptilolite Subgroup | (Na/Ca/K)3-6[Al6-7Si29-30O72] · 20H2O | |
| Cowlesite | CaAl2Si3O10 · 6H2O | Orth. mmm(2/m2/m2/m) |
| Dachiardite Subgroup | Zeolite Group. | |
| Direnzoite | NaK6MgCa2(Al13Si47O120) · 36H2O | Orth. mmm(2/m2/m2/m) : Pmmn |
| Edingtonite | Ba[Al2Si3O10] · 4H2O | Orth. 222 : P212121 |
| Epistilbite | CaAl2Si6O16 · 5H2O | Mon. |
| Erionite Subgroup | M2[Al4Si14O36] · 15H2O | |
| Fabrièsite | Na3Al3Si3O12 · 2H2O | Orth. mm2 : Pmm2 |
| Faujasite Subgroup | M3.5[Al7Si17O48] · 32H2O | |
| Ferrierite Subgroup | Name used for unanalysed specimens that could be either ferrierite-K, ferrierite-Mg, ... | |
| Ferrochiavennite | Ca1-2Fe[(Si,Al,Be)5Be2O13(OH)2] · 2H2O | Mon. 2/m : P21/b |
| Flörkeite | (K3Ca2Na)[Al8Si8O32] · 12H2O | Tric. 1 : P1 |
| Garronite Subgroup | ||
| Gaultite | Na4Zn2Si7O18 · 5H2O | Orth. mm2 : Fdd2 |
| 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. mmm(2/m2/m2/m) : Pnma |
| Goosecreekite | Ca[Al2Si6O16] · 5H2O | Mon. 2 : P21 |
| Gottardiite | Na3Mg3Ca5Al19Si117O272 · 93H2O | Orth. mmm(2/m2/m2/m) : Cmca |
| Heulandite Subgroup | (Na/Ca/K)5-6[Al8-9 Si27-28 O72] · nH2O | |
| Hsianghualite | Ca3Li2(Be3Si3O12)F2 | Iso. 23 : I213 |
| Kalborsite | K6Al4BSi6O20(OH)4Cl | Tet. 42m : P421c |
| Kirchhoffite | Cs(BSi2O6) | Tet. 4/mmm(4/m2/m2/m) : I41/acd |
| Laumontite | CaAl2Si4O12 · 4H2O | Mon. 2/m : B2/m |
| Limousinite | BaCa[Be4P4O16] · 6H2O | Mon. 2/m : P21/b |
| Lithosite | K6Al4Si8O25 · 2H2O | Mon. |
| Loomisite | Ba[Be2P2O8] · H2O | Mon. m |
| Lovdarite | K2Na6Be4Si14O36 · 9H2O | Orth. mm2 |
| Maricopaite | Pb7Ca2(Si,Al)48O100 · 32H2O | Orth. |
| Martinandresite | Ba2(Al4Si12O32) · 10H2O | Orth. mmm(2/m2/m2/m) : Pmmn |
| Mazzite Subgroup | Zeolite Group. | |
| Meierite | Ba44Si66Al30O192Cl25(OH)33 | Iso. m3m(4/m32/m) : Im3m |
| Merlinoite | K5Ca2(Si23Al9)O64 · 24H2O | Orth. mmm(2/m2/m2/m) : Immm |
| Montesommaite | (K,Na)9Al9Si23O64 · 10H2O | Orth. mm2 : Fdd2 |
| Mordenite | (Na2,Ca,K2)4(Al8Si40)O96 · 28H2O | Orth. |
| Mountainite | KNa2Ca2[Si8O19(OH)] · 6H2O | Mon. 2/m : P2/b |
| Mutinaite | Na3Ca4Si85Al11O192 · 60H2O | Orth. mmm(2/m2/m2/m) : Pnma |
| Nabesite | Na2BeSi4O10 · 4H2O | Orth. 222 : P212121 |
| Natrolite Subgroup | A subgroup of the Zeolite Group. | |
| Offretite | KCaMg(Si13Al5)O36 · 15H2O | Hex. 6m2 : P6m2 |
| Pahasapaite | Li8(Ca,Li,K)10.5Be24(PO4)24 · 38H2O | Iso. 23 : I23 |
| Parthéite | Ca2(Si4Al4) O15 (OH)2 · 4H2O | Mon. 2/m : B2/b |
| Paulingite Subgroup | Paulingite was originally described in 1960. | |
| Perlialite | K9Na(Ca,Sr)[Al2Si4O12]6 · 15H2O | Hex. 6/mmm(6/m2/m2/m) : P6/mmm |
| Phillipsite Subgroup | (Ca0.5,K,Na,Ba0.5)4-7[Al4-7Si12-9O32] . 12H2O | |
| Pollucite | (Cs,Na)2(Al2Si4O12) · 2H2O | Iso. m3m(4/m32/m) : Ia3d |
| Roggianite | Ca2Be(OH)2Al2Si4O13 · 2.5H2O | Tet. 4/mmm(4/m2/m2/m) : I4/mcm |
| Rongibbsite | Pb2(Si4Al)O11(OH) | Mon. 2/m : B2/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. | |
| Thornasite | Na12Th4+3(Si8O19)4 · 18H2O | Trig. 3m : R3m |
| Tschernichite | (Ca,Na2)[Al2Si4O12] · 4-8H2O | Tet. 4/mmm(4/m2/m2/m) : P4/mmm |
| Tschörtnerite | Ca4(Ca,Sr,K,Ba)3Cu3[Al3Si3O12]4(OH)8 · nH2O | Iso. m3m(4/m32/m) : Fm3m |
| '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 : P4122 |
| 'Unnamed (Ca analogue of Merlinoite)' | (Ca,K,Na)5(Ca,Ba)2Al9Si23O64 · 23H2O ? | |
| Wairakite | Ca(Al2Si4O12) · 2H2O | Mon. 2/m : B2/m |
| Weinebeneite | CaBe3(PO4)2(OH)2 · 4H2O | Mon. m : Bb |
| Wenkite | (Ba,K)4(Ca,Na)6[(Si,Al)20O39(OH)2](SO4)3 · 0.5H2O | Hex. 6m2 : P62m |
| Wilancookite | (Ba5Li2◻)Ba6Be24P24O96 · 26H2O | Iso. 23 : I23 |
| Willhendersonite | KCa[Al3Si3O12] · 5H2O | Tric. 1 : P1 |
| Yugawaralite | CaAl2Si6O16 · 4H2O | Mon. m : Pb |
Common Associates
| 42 photos of Leucite associated with Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| 26 photos of Leucite associated with Nepheline | Na3K(Al4Si4O16) |
| 22 photos of Leucite associated with Fluorapatite | Ca5(PO4)3F |
| 18 photos of Leucite associated with Pyroxene Group | ADSi2O6 |
| 17 photos of Leucite associated with Melilite Group | Ca2M(XSiO7) |
| 15 photos of Leucite associated with Calcite | CaCO3 |
| 14 photos of Leucite associated with Magnetite | Fe2+Fe3+2O4 |
| 11 photos of Leucite associated with Perovskite | CaTiO3 |
| 6 photos of Leucite associated with Feldspar Group | |
| 5 photos of Leucite associated with Pseudobrookite | Fe3+2Ti4+O5 |
Related Minerals - Strunz-mindat Grouping
| 9.GB.05 | Fabrièsite | Na3Al3Si3O12 · 2H2O |
| 9.GB.05 | Lithosite | K6Al4Si8O25 · 2H2O |
| 9.GB.05 | Wairakite | Ca(Al2Si4O12) · 2H2O |
| 9.GB.05 | Kirchhoffite | Cs(BSi2O6) |
| 9.GB.05 | Hsianghualite | Ca3Li2(Be3Si3O12)F2 |
| 9.GB.05 | Pollucite | (Cs,Na)2(Al2Si4O12) · 2H2O |
| 9.GB.05 | Ammonioleucite | (NH4)(AlSi2O6) |
| 9.GB.05 | Analcime | Na(AlSi2O6) · H2O |
| 9.GB.10 | Laumontite | CaAl2Si4O12 · 4H2O |
| 9.GB.15 | Yugawaralite | CaAl2Si6O16 · 4H2O |
| 9.GB.20 | Roggianite | Ca2Be(OH)2Al2Si4O13 · 2.5H2O |
| 9.GB.25 | Goosecreekite | Ca[Al2Si6O16] · 5H2O |
| 9.GB.30 | Montesommaite | (K,Na)9Al9Si23O64 · 10H2O |
| 9.GB.35 | Parthéite | Ca2(Si4Al4) O15 (OH)2 · 4H2O |
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) | 17.9147% | 5,554 | 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.
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: –
| Distance | Dose rate | Risk |
|---|---|---|
| 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 Information
Leucite in petrology
Internet Links for Leucite
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References for Leucite
Localities for Leucite
Showing 447 localities.
Locality List
- 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).
All localities listed without proper references should be considered as questionable.






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Mount Vesuvius, Metropolitan City of Naples, Campania, Italy