Rock Identifier
Polished brecciated jasper pebble (Microcrystalline quartz (SiO₂), with iron-oxide inclusions) — mineral
mineral

Polished brecciated jasper pebble

Microcrystalline quartz (SiO₂), with iron-oxide inclusions

AI-generated identification · may be incorrect

Opaque cream, tan, black, and reddish-brown material with a polished/worn surface and waxy to dull luster; quartz hardness is about 6.5–7 Mohs, with no visible cleavage and cryptocrystalline structure. The dark patches are likely manganese or iron oxides, though exact identification requires testing.

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Physical properties

Opaque cream, tan, black, and reddish-brown material with a polished/worn surface and waxy to dull luster; quartz hardness is about 6.5–7 Mohs, with no visible cleavage and cryptocrystalline structure. The dark patches are likely manganese or iron oxides, though exact identification requires testing.

Formation & geological history

Jasper forms when silica-rich fluids replace or cement fine sediments or volcanic material, commonly producing brecciation and iron-oxide coloration. It may range from Precambrian to much younger ages, depending on its deposit.

Uses & applications

Used as ornamental stone, cabochons, beads, carvings, and lapidary specimens; small polished pebbles generally have modest value.

Geological facts

Jasper is a variety of chalcedony/microcrystalline quartz rather than a single mineral species. Its mottled patterns are natural and often enhanced by polishing.

Field identification & locations

Field clues include opacity, fine grain, glassy-to-waxy fracture, and resistance to scratching; it should not be scratched with a steel knife easily. Common sources include India, Madagascar, Brazil, Australia, and the western United States.