Rock Identifier
Tumbled amber-colored quartz/chalcedony (Microcrystalline quartz (SiO₂), possibly iron-stained chalcedony or carnelian) — mineral
mineral

Tumbled amber-colored quartz/chalcedony

Microcrystalline quartz (SiO₂), possibly iron-stained chalcedony or carnelian

AI-generated identification · may be incorrect

Mohs hardness 6.5–7; translucent honey-brown to orange, with a waxy-to-glassy luster and no obvious cleavage. Rounded, polished surfaces and possible internal cloudiness are consistent with tumbled chalcedony; the photograph is insufficient for certainty.

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Physical properties

Mohs hardness 6.5–7; translucent honey-brown to orange, with a waxy-to-glassy luster and no obvious cleavage. Rounded, polished surfaces and possible internal cloudiness are consistent with tumbled chalcedony; the photograph is insufficient for certainty.

Formation & geological history

Forms when silica-rich fluids fill cavities or fractures, later crystallizing as chalcedony; iron impurities can produce orange-brown color. Such material commonly formed in volcanic rocks during the Cenozoic or older geological periods.

Uses & applications

Used for inexpensive cabochons, beads, carvings, and decorative tumbled stones; common pieces generally have modest value.

Geological facts

A scratch test against ordinary steel or a streak test on unglazed porcelain can help distinguish quartz from softer amber or resin, but these tests may damage the specimen.

Field identification & locations

Common sources include Brazil, Uruguay, India, Madagascar, and the western United States. Inspect for quartz-like hardness, cool stone feel, and lack of amber’s electrostatic attraction; definitive identification may require refractive-index or specific-gravity testing.