
mineral
Polished jasper (likely brecciated or orbicular jasper)
Jasper, microcrystalline quartz (SiO₂) with iron-oxide and other mineral impurities
AI-generated identification · may be incorrectTypically hardness 6.5–7 Mohs, opaque, waxy to dull/vitreous luster, and red-brown, cream, gray, or yellow coloration from iron oxides. It has no visible cleavage and a dense, fine-grained cryptocrystalline structure; the rounded shape indicates tumbling or polishing.
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Physical properties
Typically hardness 6.5–7 Mohs, opaque, waxy to dull/vitreous luster, and red-brown, cream, gray, or yellow coloration from iron oxides. It has no visible cleavage and a dense, fine-grained cryptocrystalline structure; the rounded shape indicates tumbling or polishing.
Formation & geological history
Jasper forms when silica-rich groundwater replaces or fills cavities and fractures in volcanic or sedimentary rocks, incorporating iron oxides and breccia fragments. Formation ages vary widely, commonly from Paleozoic to Cenozoic deposits.
Uses & applications
Used for cabochons, beads, carvings, decorative stones, and lapidary collections; occasionally used as ornamental stone. It is generally valued for pattern and polish rather than rarity.
Geological facts
The mottled red-and-cream pattern is characteristic of iron-rich jasper, though exact identification requires examination of texture and locality. Jasper is a variety of chalcedony or microcrystalline quartz, not a single mineral species.
Field identification & locations
Common in volcanic terrains and sedimentary iron- and silica-rich deposits worldwide, including Australia, Brazil, India, Madagascar, Mexico, and the western United States. Field clues include opacity, fine texture, strong polish, and resistance to scratching by steel.
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