
mineral
Polished labradorite
Labradorite, a calcic plagioclase feldspar; approximately (Ca,Na)(Al,Si)₄O₈
AI-generated identification · may be incorrectHardness 6–6.5 Mohs; gray to brown body color with polished vitreous luster and subtle blue-green iridescence (labradorescence). It has triclinic crystal structure and two cleavage directions, though the pictured tumbled piece has rounded edges.
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Physical properties
Hardness 6–6.5 Mohs; gray to brown body color with polished vitreous luster and subtle blue-green iridescence (labradorescence). It has triclinic crystal structure and two cleavage directions, though the pictured tumbled piece has rounded edges.
Formation & geological history
Forms in mafic igneous rocks such as gabbro, basalt, and anorthosite as magma cools; its exact geological age depends on locality, with major deposits ranging from Precambrian to younger formations.
Uses & applications
Used as ornamental stone, cabochons, beads, polished décor, and occasionally architectural facing; this specimen is jewelry/collecting material rather than a structural rock.
Geological facts
Its internal lamellar twinning produces interference colors when light enters at the proper angle; the subdued flash here may reflect orientation, surface finish, or lower-grade material.
Field identification & locations
Identify it by gray feldspar appearance, strong cleavage, hardness near steel nail/glass range, and blue-green or gold flashes when tilted under a focused light. Common sources include Labrador, Canada; Finland; Madagascar; Norway; and Ukraine.
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