
mineral
Labradorite
(Ca, Na)(Al, Si)4O8
Hardness: 6-6.5 on Mohs scale. Color: Gray to smoky black base with labradorescence (blue, green, yellow, orange flashes). Luster: Vitreous to pearly. Crystal structure: Triclinic. Cleavage: Perfect in two directions.
- Hardness
- 6-6
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 6-6.5 on Mohs scale. Color: Gray to smoky black base with labradorescence (blue, green, yellow, orange flashes). Luster: Vitreous to pearly. Crystal structure: Triclinic. Cleavage: Perfect in two directions.
Formation & geological history
Formed in mafic igneous rocks such as basalt and gabbro. It is an intermediate to calcic member of the plagioclase feldspar series, typically crystallizing at high temperatures within cooling magma bodies.
Uses & applications
Primarily used as a gemstone in jewelry, ornamental carvings, and high-end architectural tiles or countertops. It is also a popular specimen for crystal healing collectors.
Geological facts
Labradorite is famous for its optical effect known as labradorescence, which is caused by light diffraction within internal lamellar structures. Legend says the Northern Lights were once trapped in the rocks along the coast of Labrador until a warrior struck them with a spear.
Field identification & locations
Identified by its unique iridescent play of color when rotated under light. Look for dark, dull-looking gray rocks that suddenly flash bright blue or gold. Large deposits are found in Canada (Labrador), Madagascar, Finland, and Russia.
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Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Sandstone with Mineral Veining or Crust
Sedimentary Sandstone (mostly SiO2 with Fe2O3 tinting)
sedimentary
Schist
Schist
Metamorphic
Potassium Feldspar (Orthoclase)
Orthoclase (KAlSi3O8)
mineral
Gypsum (variety Selenite or Alabaster)
Calcium sulfate dihydrate (CaSO4·2H2O)
Mineral
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic