mineral

Weathered quartz-rich pebble

Likely quartz-bearing granitoid or quartz vein fragment; exact identification requires testing

AI-generated identification · may be incorrect

Hardness likely 6–7 Mohs, pale gray-white with brown surface staining, dull to weakly vitreous luster, and no obvious cleavage; rounded by natural abrasion. The dark patches may be iron oxides, mica, or weathered inclusions.

Identified August 25, 2026More mineral →

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Physical properties

Formation & geological history

Probably a naturally weathered and water-rounded fragment from a granitic or quartz-vein source; its geological age cannot be determined visually and may range from Precambrian to much younger. The specimen shows no clear evidence of being a fossil or meteorite.

Uses & applications

Suitable mainly as a curiosity or teaching specimen; comparable common pebbles have negligible industrial or jewelry use. It could be polished if sufficiently quartz-rich, but is unlikely to have gem value.

Geological facts

Quartz-rich rocks commonly resist weathering while softer minerals erode away, producing rounded durable pebbles. A streak, hardness, density, and close inspection of fresh surfaces would improve identification.

Field identification & locations

Common in stream gravels, beaches, glacial deposits, and landscapes underlain by granite or metamorphic rocks. Scratch testing with a steel file or glass, plus a 10× lens, can distinguish quartz from softer carbonate or ceramic material.