
mineral
Labradorite
Plagioclase Feldspar (Na,Ca)(Al,Si)4O8
AI-generated identification · may be incorrectHardness of 6 to 6.5 on the Mohs scale, grayish-green to dark gray body color with characteristic iridescent optical phenomenon called labradorescence (flashes of blue, green, gold, and copper), vitreous to pearly luster, triclinic crystal system, perfect cleavage in two directions.
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Physical properties
Hardness of 6 to 6.5 on the Mohs scale, grayish-green to dark gray body color with characteristic iridescent optical phenomenon called labradorescence (flashes of blue, green, gold, and copper), vitreous to pearly luster, triclinic crystal system, perfect cleavage in two directions.
Formation & geological history
Forms primarily in mafic igneous rocks such as basalt, gabbro, and anorthosite, as well as in some metamorphic and syenitic rocks through slow cooling of magma deep within the Earth's crust.
Uses & applications
Widely used as a gemstone in rings, pendants, and other jewelry due to its captivating optical play of colors, as well as being a popular ornamental and decorative stone.
Geological facts
Labradorite was first discovered in Paul Island near Illuak, Labrador, in Canada in 1770, which is where its name originates. Inuit legends claim that the Northern Lights were trapped inside the rocks along the coast of Labrador until a brave warrior freed most of them with a spear strike.
Field identification & locations
Readily identified by its dark, unassuming appearance from certain angles that abruptly transforms into vibrant, metallic flashes of rainbow colors when turned in the light. Major sources include Canada, Madagascar, Finland, Australia, and Russia.
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