
sedimentary
Rounded quartz-rich pebble
Likely quartzite or fine-grained quartz sandstone; exact identification requires testing
AI-generated identification · may be incorrectCream-white, opaque, smoothly water-worn, with a matte to slightly waxy luster and granular texture. Likely hardness about 6.5–7 Mohs; no visible cleavage, low porosity, and moderate specific gravity near 2.6.
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Physical properties
Cream-white, opaque, smoothly water-worn, with a matte to slightly waxy luster and granular texture. Likely hardness about 6.5–7 Mohs; no visible cleavage, low porosity, and moderate specific gravity near 2.6.
Formation & geological history
Probably formed from quartz-rich sedimentary material that was cemented or metamorphosed, then rounded by stream or beach transport. Its precise geological age and source cannot be determined from the image.
Uses & applications
Commonly collected as a curiosity, craft stone, or landscaping pebble; unsuitable for precise gemstone valuation without testing. Quartzite may be used as aggregate, paving, or building stone.
Geological facts
The rounded outline indicates prolonged abrasion by water or sediment. A steel file should not scratch quartzite, while a glass plate may be scratched by its surface.
Field identification & locations
Look for gritty quartz grains, absence of fizz with dilute hydrochloric acid, and hardness greater than ordinary limestone; a streak test is generally white. Common in riverbeds, beaches, glacial deposits, and gravel fields worldwide.
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