
mineral
Polished dark stone, likely labradorite or dark agate
Likely feldspar-rich labradorite (plagioclase) or microcrystalline quartz (chalcedony); exact identification requires testing
AI-generated identification · may be incorrectSmooth tumbled/polished surface; dark brown-gray color with pale linear veining and subvitreous-to-waxy luster. Likely hardness 6–6.5 (labradorite) or about 7 (agate); no cleavage is visible.
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Physical properties
Smooth tumbled/polished surface; dark brown-gray color with pale linear veining and subvitreous-to-waxy luster. Likely hardness 6–6.5 (labradorite) or about 7 (agate); no cleavage is visible.
Formation & geological history
Labradorite forms in slowly cooled mafic igneous rocks, while agate forms as silica-filled cavities in volcanic rocks, commonly during the Precambrian to Phanerozoic. The specimen has been cut and polished.
Uses & applications
Used as a lapidary stone for cabochons, carvings, beads, and collectibles; not typically used in construction in this small polished form.
Geological facts
Labradorite commonly shows blue, green, or gold iridescent flashes, which are not obvious here; agate usually shows curved or concentric banding. A streak, hardness, and refractive-index test would distinguish them.
Field identification & locations
Common sources include Madagascar, India, Brazil, Mexico, and the United States. Check for feldspar cleavage and flash under angled light, or quartz-like hardness and waxy conchoidal fracture for agate.