Perry Petalite prospect, Peru, Oxford Co., Maine, USA
NaAlSi3O8
Crystal System: triclinic
Colour: white to grey, bluish, greenish or reddish
Lustre: vitreous
Habitus: tabular
Hardness: 6 - 6½
Fracture: irregular/uneven or conchoidal
Cleavage: perfect on {001}, good on {010}, imperfect on {110}
Density: 2.615(6) g/cm3
Origin and geological occurrence: it belongs to the feldspar group, in particular to the plagioclase series. Albite is one of the main constituent of granites and granite pegmatites, alkali diorites, basalts and hydrothermal and alpine veins. It may be the product of sodium metasomatism. It is a typical mineral of low-grade metamorphic rocks
Samples:
9F.4 Albite #Tectosilicates |