Rock Identifier
Tumbled carnelian/chalcedony (probable) (Microcrystalline quartz, SiO₂; orange-red variety commonly called carnelian) — gemstone
gemstone

Tumbled carnelian/chalcedony (probable)

Microcrystalline quartz, SiO₂; orange-red variety commonly called carnelian

AI-generated identification · may be incorrect

Small polished pebble with translucent orange-brown coloration, gray/white edge, and waxy-to-glassy luster. Quartz hardness is about 7 Mohs; no visible cleavage, cryptocrystalline structure, and specific gravity near 2.60–2.65.

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Physical properties

Small polished pebble with translucent orange-brown coloration, gray/white edge, and waxy-to-glassy luster. Quartz hardness is about 7 Mohs; no visible cleavage, cryptocrystalline structure, and specific gravity near 2.60–2.65.

Formation & geological history

Forms when silica-rich groundwater fills cavities or replaces material in volcanic rocks, with iron impurities producing orange-red color. Its exact geological age cannot be determined visually; the Rochester region commonly exposes glacially transported Paleozoic sedimentary-derived stones.

Uses & applications

Used for beads, cabochons, jewelry, ornamental objects, and inexpensive polished-stone collections. Common tumbled pieces typically have modest value.

Geological facts

The color can deepen after heating or dyeing, so treatment cannot be ruled out from the photograph. The specimen may also be orange jasper or sard, both closely related chalcedony varieties.

Field identification & locations

Identify with a consistent waxy luster, translucency at thin edges, lack of cleavage, and hardness sufficient to scratch ordinary glass; avoid scratching valuable surfaces. Carnelian is widespread in volcanic terrains and is often sold as imported tumbled material, so local discovery does not establish local origin.