Rock Identifier
Tumbled honey-brown chalcedony (likely agate) (Microcrystalline quartz, SiO₂; chalcedony, possibly iron-stained agate) — mineral
mineral

Tumbled honey-brown chalcedony (likely agate)

Microcrystalline quartz, SiO₂; chalcedony, possibly iron-stained agate

AI-generated identification · may be incorrect

Rounded, polished, mottled golden-brown and gray with a waxy-to-glassy luster. Quartz hardness is 6.5–7 Mohs; trigonal crystal structure at the microscopic scale, with no visible cleavage and conchoidal fracture.

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Physical properties

Rounded, polished, mottled golden-brown and gray with a waxy-to-glassy luster. Quartz hardness is 6.5–7 Mohs; trigonal crystal structure at the microscopic scale, with no visible cleavage and conchoidal fracture.

Formation & geological history

Silica-rich fluids deposited quartz in rock cavities or fractures; iron oxides can create the brown and yellow coloration. The specimen’s geological age and exact source cannot be determined from the image.

Uses & applications

Tumbled chalcedony and agate are used in jewelry, ornaments, and lapidary collections; chalcedony also has limited industrial uses.

Geological facts

Agate is banded chalcedony, but banding is not clearly visible here, so the exact variety is uncertain.

Field identification & locations

Look for a hard, compact silica stone, waxy luster, and conchoidal fracture; agate may show distinct bands when held to light. Chalcedony occurs worldwide, commonly in volcanic rocks and sedimentary deposits.