
mineral
Brown chalcedony (likely carnelian/amber-like jasper)
Microcrystalline quartz, SiO₂; brown coloration commonly from iron oxides/hydroxides
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; translucent to opaque brown, resinous-to-waxy luster, cryptocrystalline structure, and no visible cleavage. The rounded, glossy surface suggests a naturally water-worn or polished piece.
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Physical properties
Hardness about 6.5–7 Mohs; translucent to opaque brown, resinous-to-waxy luster, cryptocrystalline structure, and no visible cleavage. The rounded, glossy surface suggests a naturally water-worn or polished piece.
Formation & geological history
Forms when silica-rich groundwater fills cavities and fractures, later incorporating iron staining; it may occur in volcanic rocks, gravels, and sedimentary environments. Exact age cannot be determined from the photograph.
Uses & applications
Used as decorative stone, cabochons, beads, and small carvings; attractive specimens are collected, though this piece appears common and modestly valuable.
Geological facts
Its appearance can resemble amber, brown jasper, or weathered glass. Unlike amber, chalcedony is substantially harder and usually feels cool and stone-like rather than lightweight or warm.
Field identification & locations
Look for a waxy luster, conchoidal fracture, translucency at thin edges, and resistance to scratching by steel; quartz should not be scratched by a steel knife. Common sources include Brazil, Uruguay, India, Madagascar, Mexico, and the western United States.
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