Rock Identifier
Amber-colored chalcedony (carnelian), possibly amber (Chalcedony: microcrystalline quartz (SiO₂); amber: fossilized tree resin) — mineral
mineral

Amber-colored chalcedony (carnelian), possibly amber

Chalcedony: microcrystalline quartz (SiO₂); amber: fossilized tree resin

AI-generated identification · may be incorrect

Translucent orange-brown, waxy to vitreous luster, conchoidal fracture, no cleavage; chalcedony hardness ~6.5–7 Mohs and specific gravity ~2.6. The image most strongly suggests rough carnelian/chalcedony, though amber is a visual possibility.

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Physical properties

Translucent orange-brown, waxy to vitreous luster, conchoidal fracture, no cleavage; chalcedony hardness ~6.5–7 Mohs and specific gravity ~2.6. The image most strongly suggests rough carnelian/chalcedony, though amber is a visual possibility.

Formation & geological history

Carnelian forms when silica-rich groundwater fills cavities and fractures in volcanic or sedimentary rocks, commonly in Cenozoic to older formations. Amber formed from fossilized resin, typically tens of millions of years old.

Uses & applications

Carnelian is used for beads, cabochons, carvings, and ornamental objects; amber is used in jewelry and scientific/collector specimens. Neither is generally a major construction material.

Geological facts

Carnelian is orange chalcedony colored mainly by iron impurities. Amber is much lighter (specific gravity ~1.05–1.10), warm to the touch, and may float in salt water; it can smell resinous when gently warmed.

Field identification & locations

Test cautiously: chalcedony scratches glass and feels stone-dense, whereas amber is easily scratched by steel and may show resin inclusions. Common sources include India, Brazil, Uruguay, Madagascar, and the Baltic region.