
gemstone
Tumbled amber-like chalcedony or resinous fossil material
Likely chalcedony (microcrystalline SiO₂), though the appearance could also indicate copal/amber
AI-generated identification · may be incorrectTranslucent honey-brown, smooth tumbled surface, vitreous-to-waxy luster, and no visible crystal faces; chalcedony has Mohs hardness 6.5–7, while amber/copal is much softer (about 2–3).
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Physical properties
Translucent honey-brown, smooth tumbled surface, vitreous-to-waxy luster, and no visible crystal faces; chalcedony has Mohs hardness 6.5–7, while amber/copal is much softer (about 2–3).
Formation & geological history
If chalcedony, it formed when silica-rich groundwater filled cavities or fractures and solidified over geological time; if amber, it is fossilized tree resin, commonly tens of millions of years old.
Uses & applications
Used as a lapidary and ornamental stone, in beads and carvings; amber is also used in jewelry and collectibles. The specimen is too small and visually uncertain for construction use.
Geological facts
The green flecks may be inclusions such as chlorite, plant matter, or mineral staining. A hot-needle test can damage amber and should be avoided; chalcedony commonly scratches glass, whereas amber does not.
Field identification & locations
Common chalcedony sources include Brazil, Uruguay, India, Madagascar, and the western United States; amber is notable from the Baltic region and Dominican Republic. Exact identification requires hardness, density, UV, and magnification tests.
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