
mineral
Tumbled chalcedony or quartz pebble
Microcrystalline quartz, SiO₂ (likely chalcedony); exact identification is uncertain from the image
AI-generated identification · may be incorrectRounded, 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.
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