Eucryptite
| Eucryptite | |
|---|---|
|
Eucryptite grains in albite from the type locality (size:9.3 x 7.0 x 2.8 cm) | |
| General | |
| Category | Silicate mineral |
| Formula (repeating unit) | LiAlSiO4 |
| Crystal symmetry | Trigonal 3 |
| Unit cell | a = 13.48 Å, c = 9.01 Å; Z = 18 |
| Identification | |
| Color | Brown, colorless, white |
| Crystal habit | Rare as euhedral crystals, coarse crystalline aggregates and massive |
| Crystal system | Trigonal rhombohedral |
| Cleavage | Indistinct on {1010} and {0001} |
| Fracture | Conchoidal |
| Tenacity | Very brittle |
| Mohs scale hardness | 6.5 |
| Luster | Vitreous |
| Streak | White |
| Diaphaneity | Transparent to translucent |
| Density | 2.67 |
| Optical properties | Uniaxial (+) |
| Refractive index | nω = 1.570 - 1.573 nε = 1.583 - 1.587 |
| Birefringence | δ = 0.013 |
| Other characteristics | Fluoresces pink to red or orange under SW UV |
| References | [1][2][3] |
Eucryptite is a lithium bearing aluminium silicate mineral with formula LiAlSiO4. It crystallizes in the trigonal - rhombohedral crystal system. It typically occurs as granular to massive in form and may pseudomorphically replace spodumene. It has a brittle to conchoidal fracture and indistinct cleavage. It is transparent to translucent and varies from colorless to white to brown. It has a Mohs hardness of 6.5 and a specific gravity of 2.67. Optically it is uniaxial positive with refractive index values of nω = 1.570 - 1.573 and nε = 1.583 - 1.587.
Its typical occurrence is in lithium-rich pegmatites in association with albite, spodumene, petalite, amblygonite, lepidolite and quartz.[2]
It occurs as a secondary alteration product of spodumene. It was first described in 1880 for an occurrence at its type locality, Branchville, Connecticut.[1] Its name was from the Greek for well concealed, for its typical occurrence embedded in albite.[1][2]