
mineral
Tumbled brown stone, possibly amber or polished agate
Indeterminate from image; possibilities include amber (fossilized plant resin, organic) or chalcedony/quartz (SiO₂)
AI-generated identification · may be incorrectSmall smooth rounded specimen with translucent brown-golden color and subdued waxy luster. If chalcedony, hardness is about 6.5–7 Mohs; amber is much softer at 2–2.5 and may feel unusually light.
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Physical properties
Small smooth rounded specimen with translucent brown-golden color and subdued waxy luster. If chalcedony, hardness is about 6.5–7 Mohs; amber is much softer at 2–2.5 and may feel unusually light.
Formation & geological history
Amber formed from fossilized tree resin, commonly tens of millions of years old; brown chalcedony formed when silica-rich fluids filled cavities, usually in volcanic rocks. The image lacks diagnostic detail for a confident identification.
Uses & applications
Amber is used in jewelry and collecting; chalcedony is used for cabochons, beads, carvings, and ornamental objects. Value depends strongly on transparency, inclusions, size, and treatment.
Geological facts
Amber can float in saturated salt water, attract lightweight fibers when rubbed, and smell resinous when gently warmed; quartz-based stones will not. A UV lamp may produce fluorescence in some amber, but this test is not definitive.
Field identification & locations
Common amber sources include the Baltic region and the Dominican Republic; chalcedony occurs worldwide. Examine translucency, inclusions, weight, hardness, and streak, avoiding destructive tests on an unknown specimen.
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