Labradorite

Labradorite
Labradorite in a polished rock slab
General
CategoryAdularescence, tectosilicate
Formula
(repeating unit)
(Ca,Na)(Al,Si)4O8, where Na is 30-50% & Ca is 50–70%
Crystal systemTriclinic
Crystal classPinacoidal (1)
(same H-M symbol)
Unit cella = 8.155 Å, b = 12.84 Å
c = 10.16 Å; α = 93.5°
β = 116.25°, γ = 89.133°; Z = 6
Identification
ColorGray, gray-white, brown, greenish, pale green, blue, orange, pink, yellow, colorless
Crystal habitCrystals typically thin and tabular, rhombic in cross section, striated; massive
TwinningCommon by albite, pericline, Carlsbad, Baveno, or Manebach twin laws
CleavagePerfect on {001}, less perfect on {010}, intersecting at near 90°; distinct on {110}
FractureUneven to conchoidal
Mohs scale hardness6–6.5
LusterVitreous to pearly on cleavages
StreakWhite
DiaphaneityTranslucent to transparent
Specific gravity2.68 to 2.72
Optical propertiesBiaxial (+)
Refractive indexnα = 1.554–1.563
nβ = 1.559–1.568
nγ = 1.562–1.573
Birefringenceδ = 0.008–0.010
2V angleMeasured: 85°
DispersionNone
Other characteristicsLabradorescence (iridescence, schiller optical effect)
References[1][2][3]

Labradorite ((Ca, Na)(Al, Si)4O8) is a calcium-enriched feldspar mineral first identified in Labrador, Canada, which can display an iridescent effect (schiller).

Labradorite is an intermediate to calcic member of the plagioclase series. It has an anorthite percentage (%An) of between 50 and 70. The specific gravity ranges from 2.68 to 2.72. The streak is white, like most silicates. The refractive index ranges from 1.559 to 1.573 and twinning is common. As with all plagioclase members, the crystal system is triclinic, and three directions of cleavage are present, two of which are nearly at right angles and are more obvious, being of good to perfect quality (while the third direction is poor). It occurs as clear, white to gray, blocky to lath shaped grains in common mafic igneous rocks such as basalt and gabbro, as well as in anorthosites.