
mineral
Labradorite (in Matrix)
Labradorite ((Ca, Na)(Al, Si)4O8)
Hardness: 6-6.5 on Mohs scale; Color: Gray to dark gray with metallic IRIDESCENCE (labradorescence) in blue, green, or gold; Luster: Vitreous to pearly; Crystal structure: Triclinic; Cleavage: Two directions at nearly 90 degrees.
- Hardness
- 6-6
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 6-6.5 on Mohs scale; Color: Gray to dark gray with metallic IRIDESCENCE (labradorescence) in blue, green, or gold; Luster: Vitreous to pearly; Crystal structure: Triclinic; Cleavage: Two directions at nearly 90 degrees.
Formation & geological history
Forms in mafic igneous rocks such as basalt and gabbro through the crystallization of magma. It is a calcium-enriched feldspar mineral that develops a lamellar structure during cooling, causing light interference.
Uses & applications
Widely used as a gemstone in jewelry, decorative stone for countertops or tiles, and as a popular collector's mineral.
Geological facts
The unique play of color is known as 'labradorescence,' caused by internal light reflections from submicroscopic planes oriented in one direction. It was first discovered in Labrador, Canada, in 1770.
Field identification & locations
Identify by rotating the stone under a light source to reveal the hidden 'flash' of color. Often found in Canada, Madagascar, Norway, and Finland (where a high-quality variety called Spectrolite is found).
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