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'''Leucite''' (from the Greek word ''leukos'' meaning white) is a [[rock (geology)|rock]]-forming [[mineral]] of the [[feldspathoid]] group, silica-undersaturated and composed of [[potassium]] and [[aluminium]] [[Silicate minerals|tectosilicate]] KAlSi<sub>2</sub>O<sub>6</sub>. [[Crystal]]s have the form of cubic icositetrahedra but, as first observed by Sir [[David Brewster]] in 1821, they are not optically isotropic, and are therefore pseudo-cubic. [[Goniometer|Goniometric]] measurements made by [[Gerhard vom Rath]] in 1873 led him to refer the crystals to the [[tetragonal]] system. Optical investigations have since proved the crystals to be still more complex in character, and to consist of several [[orthorhombic]] or [[monoclinic]] individuals, which are optically biaxial and repeatedly [[Crystal twinning|twinned]], giving rise to twin-lamellae and to striations on the faces. When the crystals are raised to a temperature of about 500 °C they become optically isotropic and the twin-lamellae and striations disappear, although they reappear when the crystals are cooled again. This pseudo-cubic character of leucite is very similar to that of the mineral [[boracite]]. |
'''Leucite''' (from the Greek word ''leukos'' meaning white) is a [[rock (geology)|rock]]-forming [[mineral]] of the [[feldspathoid]] group, silica-undersaturated and composed of [[potassium]] and [[aluminium]] [[Silicate minerals|tectosilicate]] KAlSi<sub>2</sub>O<sub>6</sub>.<ref>{{Cite book |title=Rocks and Minerals |publisher=[[DK Publishers]] |year=2012 |isbn=978 1 4093 8659 9 |editor-last=Star |editor-first=Fleur}}</ref> [[Crystal]]s have the form of cubic icositetrahedra but, as first observed by Sir [[David Brewster]] in 1821, they are not optically isotropic, and are therefore pseudo-cubic. [[Goniometer|Goniometric]] measurements made by [[Gerhard vom Rath]] in 1873 led him to refer the crystals to the [[tetragonal]] system. Optical investigations have since proved the crystals to be still more complex in character, and to consist of several [[orthorhombic]] or [[monoclinic]] individuals, which are optically biaxial and repeatedly [[Crystal twinning|twinned]], giving rise to twin-lamellae and to striations on the faces. When the crystals are raised to a temperature of about 500 °C they become optically isotropic and the twin-lamellae and striations disappear, although they reappear when the crystals are cooled again. This pseudo-cubic character of leucite is very similar to that of the mineral [[boracite]]. |
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The crystals are white or ash-grey in colour, hence the name suggested by [[A. G. Werner]] in 1701, from ''λευκος'', '(matt) white'. They are transparent and glassy when fresh, albeit with a noticeably subdued 'subvitreous' lustre due to the low refractive index, but readily alter to become waxy/greasy and then dull and opaque; they are brittle and break with a conchoidal fracture. The [[Mohs hardness]] is 5.5, and the [[specific gravity]] 2.47. Inclusions of other minerals, arranged in concentric zones, are frequently present in the crystals. On account of the color and form of the crystals the mineral was early known as 'white garnet'. French authors in older literature may employ [[René Just Haüy]]'s name '''''amphigène''''', but 'leucite' is the only name for this mineral species that is recognised as official by the International Mineralogical Association. |
The crystals are white or ash-grey in colour, hence the name suggested by [[A. G. Werner]] in 1701, from ''λευκος'', '(matt) white'. They are transparent and glassy when fresh, albeit with a noticeably subdued 'subvitreous' lustre due to the low refractive index, but readily alter to become waxy/greasy and then dull and opaque; they are brittle and break with a conchoidal fracture. The [[Mohs hardness]] is 5.5, and the [[specific gravity]] 2.47. Inclusions of other minerals, arranged in concentric zones, are frequently present in the crystals. On account of the color and form of the crystals the mineral was early known as 'white garnet'. French authors in older literature may employ [[René Just Haüy]]'s name '''''amphigène''''', but 'leucite' is the only name for this mineral species that is recognised as official by the International Mineralogical Association. |
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Revision as of 12:11, 2 February 2023
| Leucite | |
|---|---|
 Leucite crystals in a rock from Italy | |
| Allgemein | |
| Kategorie | tectosilicates |
| Formula (repeating unit) | KAlSi2O6 |
| IMA symbol | Lct[1] |
| Strunz classification | 9.GB.05 |
| Crystal system | Tetragonal |
| Crystal class | Dipyramidal (4/m) (same H-M symbol) |
| Space group | I41/a |
| Unit cell | a = 13.056, c = 13.751 [Å]; Z = 16 |
| Identification | |
| Color | White to grey |
| Crystal habit | Commonly as euhedral, pseudocubic crystals; rarely granular, massive |
| Twinning | Common and repeated on {110} and {101} |
| Cleavage | Poor on {110} |
| Fracture | Conchoidal |
| Tenacity | Brittle |
| Mohs scale hardness | 5.5 - 6 |
| Luster | Vitreous |
| Streak | White |
| Diaphaneity | Transparent to translucent |
| Specific gravity | 2.45-2.50 |
| Optical properties | Uniaxial (+) |
| Refractive index | nω = 1.508 nε = 1.509 |
| Birefringence | δ = 0.001 |
| References | [2][3] |
Leucite (from the Greek word leukos meaning white) is a rock-forming mineral of the feldspathoid group, silica-undersaturated and composed of potassium and aluminium tectosilicate KAlSi2O6.[4] Crystals have the form of cubic icositetrahedra but, as first observed by Sir David Brewster in 1821, they are not optically isotropic, and are therefore pseudo-cubic. Goniometric measurements made by Gerhard vom Rath in 1873 led him to refer the crystals to the tetragonal system. Optical investigations have since proved the crystals to be still more complex in character, and to consist of several orthorhombic or monoclinic individuals, which are optically biaxial and repeatedly twinned, giving rise to twin-lamellae and to striations on the faces. When the crystals are raised to a temperature of about 500 °C they become optically isotropic and the twin-lamellae and striations disappear, although they reappear when the crystals are cooled again. This pseudo-cubic character of leucite is very similar to that of the mineral boracite.
The crystals are white or ash-grey in colour, hence the name suggested by A. G. Werner in 1701, from λευκος, '(matt) white'. They are transparent and glassy when fresh, albeit with a noticeably subdued 'subvitreous' lustre due to the low refractive index, but readily alter to become waxy/greasy and then dull and opaque; they are brittle and break with a conchoidal fracture. The Mohs hardness is 5.5, and the specific gravity 2.47. Inclusions of other minerals, arranged in concentric zones, are frequently present in the crystals. On account of the color and form of the crystals the mineral was early known as 'white garnet'. French authors in older literature may employ René Just Haüy's name amphigène, but 'leucite' is the only name for this mineral species that is recognised as official by the International Mineralogical Association.
References
- ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
- ^ Leucite on Mindat
- ^ Handbook of Mineralogy
- ^ Star, Fleur, ed. (2012). Rocks and Minerals. DK Publishers. ISBN 978 1 4093 8659 9.
- This article incorporates text from a publication now in the public domain: Spencer, Leonard James (1911). "Leucite". In Chisholm, Hugh (ed.). Encyclopædia Britannica. Vol. 16 (11th ed.). Cambridge University Press. pp. 503–504.
