Rock Identifier
Likely tumbled quartz or chalcedony fragment (Quartz (SiO₂), possibly microcrystalline chalcedony) — mineral
mineral

Likely tumbled quartz or chalcedony fragment

Quartz (SiO₂), possibly microcrystalline chalcedony

AI-generated identification · may be incorrect

Small honey-yellow, translucent fragment with a vitreous to waxy luster and irregular fracture; quartz hardness is Mohs 7, while chalcedony is approximately 6.5–7. The image is partially obscured by textured glass, so crystal form and exact composition cannot be confirmed.

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Physical properties

Small honey-yellow, translucent fragment with a vitreous to waxy luster and irregular fracture; quartz hardness is Mohs 7, while chalcedony is approximately 6.5–7. The image is partially obscured by textured glass, so crystal form and exact composition cannot be confirmed.

Formation & geological history

Quartz forms in hydrothermal veins, cavities, and sedimentary or metamorphic settings; yellow coloration may result from iron staining or inclusions. Quartz ranges from Precambrian to modern in age and is globally widespread.

Uses & applications

Used for glass, ceramics, electronics, abrasives, countertops, and decorative specimens; attractive transparent pieces may be cut as citrine or other quartz gemstones.

Geological facts

A conchoidal fracture, lack of cleavage, and ability to scratch ordinary glass support quartz identification. Color alone is unreliable because heat treatment and iron staining can produce yellow tones.

Field identification & locations

Common sources include Brazil, Madagascar, the United States, and worldwide quartz-bearing veins; test only with care using hardness and streak tests. Likely value is $1–$10 for a small common fragment, or $10–$50 if gem-quality.