Rock Identifier
Tumbled yellow-brown translucent stones, likely quartz/chalcedony (Quartz (SiO₂) or microcrystalline quartz (chalcedony); exact identification requires testing) — mineral
mineral

Tumbled yellow-brown translucent stones, likely quartz/chalcedony

Quartz (SiO₂) or microcrystalline quartz (chalcedony); exact identification requires testing

AI-generated identification · may be incorrect

Pale honey to brown color, translucent, rounded/tumbled surfaces, vitreous to waxy luster, no visible cleavage, conchoidal fracture; quartz hardness Mohs 7 and specific gravity about 2.65.

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Physical properties

Pale honey to brown color, translucent, rounded/tumbled surfaces, vitreous to waxy luster, no visible cleavage, conchoidal fracture; quartz hardness Mohs 7 and specific gravity about 2.65.

Formation & geological history

Quartz and chalcedony form in silica-rich veins, cavities, and sedimentary environments through hydrothermal or groundwater deposition; the specimens were subsequently human-tumbled and polished.

Uses & applications

Used as inexpensive lapidary material, ornamental stones, jewelry, cabochons, and educational specimens; common pieces have little intrinsic value.

Geological facts

Yellow coloration may result from iron staining or inclusions. The image does not provide enough detail to distinguish citrine, yellow jasper, agate, or ordinary stained quartz confidently.

Field identification & locations

Commonly found in quartz veins, gravel deposits, and agate-bearing volcanic regions worldwide. A glass scratch test, streak test, and close inspection for banding or granular texture can help identify them; avoid damaging valuable pieces.