Rock Identifier
Polished brown chalcedony or jasper (Microcrystalline quartz (SiO₂), likely iron-stained chalcedony/jasper with vugs) — mineral
mineral

Polished brown chalcedony or jasper

Microcrystalline quartz (SiO₂), likely iron-stained chalcedony/jasper with vugs

AI-generated identification · may be incorrect

Hardness about 6.5–7 Mohs; reddish-brown to orange-brown, waxy to dull luster, cryptocrystalline quartz, and irregular cavities lined or filled with pale mineral material. The rounded shape appears naturally water-worn or tumbled.

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Physical properties

Hardness about 6.5–7 Mohs; reddish-brown to orange-brown, waxy to dull luster, cryptocrystalline quartz, and irregular cavities lined or filled with pale mineral material. The rounded shape appears naturally water-worn or tumbled.

Formation & geological history

Likely formed when silica-rich fluids filled or replaced volcanic rock, with iron oxides producing the brown-red color; cavities may preserve former gas bubbles or weathered inclusions. Exact age and locality cannot be determined from the photograph.

Uses & applications

Used as a lapidary stone for cabochons, carvings, polished specimens, and inexpensive jewelry; jasper is also used decoratively and occasionally in architecture.

Geological facts

The specimen may be brecciated jasper or vuggy chalcedony rather than a single precise variety. A streak, hardness, and close examination of the cavities would improve identification.

Field identification & locations

Commonly found in volcanic terrains, especially silica-rich lava flows and hydrothermal veins. It should scratch ordinary glass but not be scratched by a steel knife; fizzing in dilute acid would suggest carbonate material instead.