
mineral
Polished brecciated jasper pebble
Microcrystalline quartz (SiO₂), with iron-oxide inclusions
AI-generated identification · may be incorrectOpaque 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.
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