
mineral
Polished/tumbled jasper or chalcedony
Microcrystalline quartz (SiO₂), likely brown jasper/chalcedony
AI-generated identification · may be incorrectSmooth, highly polished brown-gold specimen with cloudy cream banding and patches. Quartz hardness is about 7 Mohs; vitreous to waxy luster, cryptocrystalline structure, no visible cleavage, and typical specific gravity near 2.6. The exact variety cannot be confirmed visually.
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Physical properties
Smooth, highly polished brown-gold specimen with cloudy cream banding and patches. Quartz hardness is about 7 Mohs; vitreous to waxy luster, cryptocrystalline structure, no visible cleavage, and typical specific gravity near 2.6. The exact variety cannot be confirmed visually.
Formation & geological history
Forms when silica-rich groundwater fills cavities or replaces rock, with iron oxides producing the brown coloration. Such material commonly formed in volcanic or sedimentary environments over geologic timescales; it is likely tumbled or cut and polished rather than naturally shaped.
Uses & applications
Used as ornamental stone, cabochons, jewelry, carvings, and polished collectibles. It is not normally used as a structural construction stone in this form.
Geological facts
The cream-and-brown appearance may also resemble iron-stained agate, petrified wood, or brown calcite, but the smooth opaque-to-translucent texture is most consistent with jasper/chalcedony. A hardness test is useful: quartz should resist scratching by a steel blade.
Field identification & locations
Commonly found as pebbles, cavity fillings, and silica-rich nodules. Brazil, including southeastern Brazil near 20.1°S, 42.0°W, is a plausible source region for varied quartz and jasper materials. Confirm with hardness, streak, translucency, and—if available—specific-gravity testing.
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