Rock Identifier
Tumbled chalcedony or quartz pebble (Microcrystalline quartz, SiO₂ (likely chalcedony); exact identification is uncertain from the image) — mineral
mineral

Tumbled chalcedony or quartz pebble

Microcrystalline quartz, SiO₂ (likely chalcedony); exact identification is uncertain from the image

AI-generated identification · may be incorrect

Rounded, polished, translucent pale olive-gray material with a waxy to vitreous luster and cloudy internal texture. Quartz has Mohs hardness 7, no cleavage, conchoidal fracture, and specific gravity about 2.65.

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Physical properties

Rounded, polished, translucent pale olive-gray material with a waxy to vitreous luster and cloudy internal texture. Quartz has Mohs hardness 7, no cleavage, conchoidal fracture, and specific gravity about 2.65.

Formation & geological history

Likely formed when silica-rich groundwater filled cavities or fractures, later weathered and naturally or artificially rounded; its geological age cannot be determined visually. The yellow-green tint may reflect iron-bearing inclusions or surface staining.

Uses & applications

Used as a lapidary, carving, and decorative stone; attractive pieces may be made into cabochons or jewelry. Common tumbled specimens have modest commercial value.

Geological facts

Chalcedony is quartz composed of extremely fine intergrowths of quartz varieties, commonly displaying translucency and a waxy surface. The specimen could also be a low-grade jasper or quartzite, which require testing for distinction.

Field identification & locations

Common in volcanic cavities, sedimentary nodules, river gravels, and silica-rich veins worldwide; test hardness against steel or glass, inspect for conchoidal fracture, and use a 10× loupe for fibrous chalcedony texture.