Rock Identifier
Tumbled yellow chalcedony (likely citrine or yellow jasper) (Microcrystalline quartz, SiO₂; exact identification is uncertain from the photograph) — mineral
mineral

Tumbled yellow chalcedony (likely citrine or yellow jasper)

Microcrystalline quartz, SiO₂; exact identification is uncertain from the photograph

AI-generated identification · may be incorrect

Hardness about 6.5–7 Mohs, waxy to vitreous luster, translucent yellow coloration, and no visible cleavage; the color may come from iron staining or inclusions. Its smooth rounded form indicates tumbling or natural water wear.

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Physical properties

Hardness about 6.5–7 Mohs, waxy to vitreous luster, translucent yellow coloration, and no visible cleavage; the color may come from iron staining or inclusions. Its smooth rounded form indicates tumbling or natural water wear.

Formation & geological history

Chalcedony forms when silica-rich fluids fill cavities and fractures, commonly in volcanic rocks; yellow varieties develop through iron impurities or alteration. Formation ages vary widely, from Cenozoic to much older deposits.

Uses & applications

Used for cabochons, beads, carvings, and inexpensive jewelry; attractive pieces are collected as lapidary stones.

Geological facts

The specimen could also be yellow calcite, resin, or dyed quartz; hardness and an acid test would help distinguish them. Quartz does not effervesce in dilute hydrochloric acid.

Field identification & locations

Common sources include Brazil, Uruguay, Madagascar, India, and the western United States. Test with a steel file or glass cautiously: quartz should scratch glass, while calcite will not and has much softer cleavage.