Eucryptite
The importance of Eucryptite in contemporary society is undeniable. Whether professionally, culturally, personally or politically, Eucryptite has a significant impact on our lives. As technology advances, Eucryptite continues to be relevant and its influence becomes increasingly evident. In this article, we will explore the role and importance of Eucryptite in different contexts, analyzing its evolution over time and its impact on the world today. Additionally, we will examine how Eucryptite has shaped the way we think, act and relate, and how we can harness its potential to promote change and progress in society.
| Eucryptite | |
|---|---|
 Eucryptite grains in albite from the type locality (size: 9.3 × 7.0 × 2.8 cm) | |
| General | |
| Category | Silicate mineral |
| Formula | LiAlSiO4 |
| IMA symbol | Ecp[1] |
| Crystal system | Trigonal |
| Crystal class | Rhombohedral (3) H-M symbol: (3) |
| Space group | R3 |
| Unit cell | a = 13.48, c = 9.01 ; Z = 18 |
| Identification | |
| Color | Brown, colorless, white |
| Crystal habit | Rare as euhedral crystals, coarse crystalline aggregates and massive |
| 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 | [2][3][4] |
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.[3]
It occurs as a secondary alteration product of spodumene. It was first described in 1880 for an occurrence at its type locality, Branchville, Connecticut.[2] Its name was from the Greek for well concealed, for its typical occurrence embedded in albite.[2][3]
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.
- ^ a b c Mindat.org
- ^ a b c Handbook of Mineralogy
- ^ Webmineral data
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