
mineral
Polished brecciated jasper or agate
Microcrystalline quartz (chalcedony), SiO₂, with iron-oxide inclusions and brecciation
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; mottled red, brown, gray, and translucent white areas; waxy to vitreous luster; cryptocrystalline quartz with no visible cleavage and conchoidal fracture. The rounded surface indicates tumbling or polishing.
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Physical properties
Hardness about 6.5–7 Mohs; mottled red, brown, gray, and translucent white areas; waxy to vitreous luster; cryptocrystalline quartz with no visible cleavage and conchoidal fracture. The rounded surface indicates tumbling or polishing.
Formation & geological history
Likely formed when silica-rich groundwater filled fractures or replaced rock, with iron oxides producing the red-brown colors; later weathering released the nodule. Precise age and locality cannot be determined from the photograph.
Uses & applications
Used as an ornamental stone, cabochon, bead, and lapidary material; attractive pieces have modest jewelry and collecting value.
Geological facts
The specimen appears brecciated, meaning angular fragments were cemented by later silica. Strong translucency and quartz-like hardness help distinguish it from ordinary opaque jasper.
Field identification & locations
Test carefully on an inconspicuous edge: it should scratch window glass but not be scratched by a steel knife. Common sources include Oregon, Idaho, Utah, Brazil, Madagascar, and Australia; exact identification requires locality or testing.
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