mineral

Polished amber-like chalcedony/jasper

Microcrystalline quartz (SiO₂), likely iron-stained chalcedony or jasper; amber cannot be confirmed visually

AI-generated identification · may be incorrect

Honey-orange to reddish-brown, translucent in thin areas, with waxy to vitreous luster and irregular fractures; quartz hardness is about Mohs 6.5–7, with no cleavage and specific gravity near 2.6.

Identified September 12, 2026More mineral →

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Physical properties

Honey-orange to reddish-brown, translucent in thin areas, with waxy to vitreous luster and irregular fractures; quartz hardness is about Mohs 6.5–7, with no cleavage and specific gravity near 2.6.

Formation & geological history

Forms when silica-rich fluids fill cavities or replace volcanic/sedimentary material, with iron oxides producing orange-red coloration; age depends on its host deposit and cannot be determined from the photograph.

Uses & applications

Used as a decorative carving or cabochon material, ornamental stone, and collector specimen; quality depends on translucency, pattern, polish, and lack of cracks.

Geological facts

The bright honey color can resemble fossil resin (amber), but amber is organic, much softer (Mohs 2–2.5), and typically lighter in density.

Field identification & locations

Look for a glassy/waxy surface, conchoidal fracture, hardness sufficient to scratch glass, and no obvious resin-like inclusions; common sources include volcanic and sedimentary silica deposits worldwide.