Rock Identifier
Polished labradorite cabochon (Labradorite, a plagioclase feldspar: (Ca,Na)(Al,Si)₄O₈) — mineral
mineral

Polished labradorite cabochon

Labradorite, a plagioclase feldspar: (Ca,Na)(Al,Si)₄O₈

AI-generated identification · may be incorrect

Likely a smooth, polished cabochon showing subdued blue-green and bronze labradorescence. Hardness 6–6.5 Mohs; vitreous luster, triclinic crystals, two cleavages near 90°, specific gravity about 2.7.

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Physical properties

Likely a smooth, polished cabochon showing subdued blue-green and bronze labradorescence. Hardness 6–6.5 Mohs; vitreous luster, triclinic crystals, two cleavages near 90°, specific gravity about 2.7.

Formation & geological history

Forms in cooling mafic igneous rocks, especially gabbro and anorthosite; its age depends on the deposit. The color flashes arise from light interference within fine internal layers of feldspar.

Uses & applications

Used in cabochon jewelry, beads, ornaments, and decorative stonework.

Geological facts

Labradorescence is the characteristic shifting color effect, often strongest when the stone is viewed from particular angles.

Field identification & locations

Common sources include Labrador, Canada; Madagascar; Finland; and Norway. Identify it by rotating the polished surface under light for angular flashes; the dark appearance in this image limits certainty.