Euclase
| Euclase | ||
|---|---|---|
2V angle 50° | | |
| Dispersion | r > v | |
| References | [2][3][4] | |
Euclase is a
monoclinic crystal system and is typically massive to fibrous as well as in slender prismatic crystals. It is related to beryl (Be3Al2Si6O18) and other beryllium minerals. It is a product of the decomposition of beryl in pegmatites.[4]
Euclase crystals are noted for their blue color, ranging from very pale to dark blue. The mineral may also be colorless, white, or light green. Cleavage is perfect, parallel to the clinopinacoid, and this suggested to René Just Haüy the name euclase, from the Greek εὖ, easily, and κλάσις, fracture. The ready cleavage renders the crystals fragile with a tendency to chip, and thus detracts from its use for personal ornament. When cut, it resembles certain kinds of beryl and topaz, from which it may be distinguished by its specific gravity (3.1). Its hardness (7.5) is similar to beryl (7.5 - 8), and a bit less than that of topaz (8).[5] It was first reported in 1792 from the
mica-schist of the Rauris
in the Austrian Alps.
References
- S2CID 235729616.
- ^ Euclase data on Webmineral
- ^ a b Euclase on Mindat.org with location data
- ^ a b Euclase in the Handbook of Mineralogy, Mineral Data Publishers PDF
- ^ Chisholm, Hugh, ed. (1911). . Encyclopædia Britannica (11th ed.). Cambridge University Press.
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