
gemstone
Polished orbicular jasper or rhyolitic jasper
Silica-rich microcrystalline quartz/chalcedony (SiO₂), likely jasper with contrasting mineral veins
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; gray-green to brown, opaque, with a waxy to vitreous polish and irregular pale vein network. Microcrystalline quartz lacks visible cleavage and commonly has specific gravity near 2.6.
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Physical properties
Hardness about 6.5–7 Mohs; gray-green to brown, opaque, with a waxy to vitreous polish and irregular pale vein network. Microcrystalline quartz lacks visible cleavage and commonly has specific gravity near 2.6.
Formation & geological history
Forms when silica-rich volcanic or sedimentary material is replaced and cemented by chalcedony/quartz, with later fractures filled by lighter minerals. Exact age cannot be determined from the image; jasper occurs in many Paleozoic–Cenozoic deposits.
Uses & applications
Used for cabochons, beads, worry stones, carvings, and ornamental objects; generally decorative rather than industrial.
Geological facts
The rounded shape and high polish indicate a human-worked tumbled or carved specimen. Similar material is often sold as “brecciated jasper,” “rhyolite jasper,” or occasionally “crocodile jasper,” though visual identification alone is uncertain.
Field identification & locations
Look for opaque fine grain, no glassy translucence, hardness sufficient to scratch ordinary glass, and natural-looking mineral veins or breccia patterns. Common sources include India, Madagascar, Indonesia, Mexico, and the western United States.
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