
mineral
Jasper (brecciated or orbicular jasper)
Microcrystalline quartz/chalcedony (SiO₂), colored by iron oxides and other impurities
AI-generated identification · may be incorrectTypically opaque, reddish-brown, gray, and cream with brecciated patches; waxy to dull luster and no visible cleavage. Mohs hardness 6.5–7; fine-grained cryptocrystalline quartz, with variable specific gravity around 2.6.
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Physical properties
Typically opaque, reddish-brown, gray, and cream with brecciated patches; waxy to dull luster and no visible cleavage. Mohs hardness 6.5–7; fine-grained cryptocrystalline quartz, with variable specific gravity around 2.6.
Formation & geological history
Forms when silica-rich groundwater fills fractures or replaces volcanic and sedimentary material, while iron oxides create red-brown coloration. Deposits range from ancient Precambrian to relatively young volcanic settings.
Uses & applications
Used as an ornamental and lapidary stone for cabochons, carvings, beads, and polished specimens; rarely used as a minor decorative aggregate.
Geological facts
Jasper is a variety of opaque chalcedony rather than a single mineral species. Brecciated varieties preserve angular fragments cemented by later silica, producing the mottled appearance.
Field identification & locations
Identify it by its opaque color patterns, glassy/waxy fracture, and inability to scratch it with a steel knife; quartz-rich jasper should scratch glass. Common in volcanic terrains and silica-rich veins worldwide.
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