
mineral
Tumbled orange-brown quartz pebble
Likely iron-stained quartz or chalcedony (SiO₂)
AI-generated identification · may be incorrectMohs hardness 6.5–7; translucent orange-brown color, waxy to vitreous luster, and microcrystalline or granular texture. The rounded surface appears tumbled and may contain iron-oxide staining or minor inclusions.
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Physical properties
Mohs hardness 6.5–7; translucent orange-brown color, waxy to vitreous luster, and microcrystalline or granular texture. The rounded surface appears tumbled and may contain iron-oxide staining or minor inclusions.
Formation & geological history
Quartz forms in igneous, hydrothermal, and sedimentary environments; iron staining commonly develops during weathering. The specimen was likely naturally rounded or mechanically tumbled, and its precise geological age cannot be determined visually.
Uses & applications
Used as a low-cost lapidary, craft, and decorative stone; comparable material may be sold as tumbled quartz, jasper, or chalcedony. It has little industrial value at this size.
Geological facts
The image cannot reliably distinguish quartz from similar hard materials such as quartz-rich jasper or iron-stained chalcedony. A glassy fracture and ability to scratch ordinary glass would support quartz identification.
Field identification & locations
Common worldwide, especially in quartz veins, river gravels, and weathered volcanic or metamorphic terrains. Confirm with a hardness test, streak test, and ideally specific gravity; avoid destructive testing on valuable specimens.
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