Rock Identifier
Polished jasper, likely brecciated or orbicular jasper (Microcrystalline quartz (chalcedony), SiO₂, with iron-oxide and other mineral impurities) — mineral
mineral

Polished jasper, likely brecciated or orbicular jasper

Microcrystalline quartz (chalcedony), SiO₂, with iron-oxide and other mineral impurities

AI-generated identification · may be incorrect

Opaque, multicolored gray, cream, orange, and brown with mottled/brecciated patterns; dull to waxy luster and no visible crystal faces. Quartz hardness is about Mohs 6.5–7; conchoidal fracture, very fine-grained structure, and typically low porosity, though the visible holes may be natural cavities.

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Physical properties

Opaque, multicolored gray, cream, orange, and brown with mottled/brecciated patterns; dull to waxy luster and no visible crystal faces. Quartz hardness is about Mohs 6.5–7; conchoidal fracture, very fine-grained structure, and typically low porosity, though the visible holes may be natural cavities.

Formation & geological history

Forms when silica-rich groundwater fills or replaces volcanic ash, fractures, or cavities, with iron oxides producing orange-brown colors. Most jasper is Cenozoic to older, but this specimen’s exact age and locality cannot be determined from the image.

Uses & applications

Used for cabochons, carvings, polished display stones, beads, and lapidary décor; occasionally used as a minor ornamental stone. It is not generally used as structural construction material.

Geological facts

Jasper is a variety of opaque chalcedony rather than a single mineral species. Strong banding or angular fragments can indicate brecciated jasper, while rounded orb-like patterns may indicate orbicular jasper.

Field identification & locations

Identify it by its opacity, fine texture, hardness, waxy surface, and resistance to scratching by steel; quartz-rich jasper can scratch glass. Common sources include India, Madagascar, Brazil, Australia, Mexico, and the western United States; exact identification requires locality or testing.