
mineral
Polished amber-like chalcedony (likely carnelian or yellow jasper)
Microcrystalline quartz, SiO₂; exact identification is uncertain from the image
AI-generated identification · may be incorrectTranslucent honey-yellow to brown, glossy vitreous luster, curved internal banding or flow-like inclusions, and no obvious cleavage; quartz hardness is about 7 Mohs and specific gravity about 2.6. The rounded, polished shape suggests a lapidary-cut specimen.
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Physical properties
Translucent honey-yellow to brown, glossy vitreous luster, curved internal banding or flow-like inclusions, and no obvious cleavage; quartz hardness is about 7 Mohs and specific gravity about 2.6. The rounded, polished shape suggests a lapidary-cut specimen.
Formation & geological history
Likely silica-rich chalcedony or jasper formed when groundwater deposited quartz in cavities or replaced volcanic/sedimentary material; ages vary widely, commonly Paleozoic to Cenozoic. If genuinely amber, it would be fossilized resin, but the appearance more strongly suggests a quartz aggregate.
Uses & applications
Used for cabochons, beads, carvings, ornamental objects, and mineral collections; jasper and chalcedony are also used as inexpensive decorative stone.
Geological facts
Strong internal banding and apparent translucency are typical of chalcedony varieties, while amber is much softer and lighter. A refractive-index, hardness, and UV test would distinguish them reliably.
Field identification & locations
Common sources include Brazil, Uruguay, India, Madagascar, Mexico, and the United States. Check for quartz hardness, cool stone-like feel, and density; amber may scratch easily with a steel point and often fluoresces blue-white under UV.
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