
sedimentary
Rounded quartz-rich pebble
Likely quartzite or quartz-bearing sandstone with iron-oxide staining
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs if quartzite; gray-brown surface, pale cream weathering rind, dull to weakly vitreous luster, and no obvious cleavage. The rounded shape and apparent granular texture suggest abrasion in stream or beach sediment.
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Physical properties
Hardness about 6.5–7 Mohs if quartzite; gray-brown surface, pale cream weathering rind, dull to weakly vitreous luster, and no obvious cleavage. The rounded shape and apparent granular texture suggest abrasion in stream or beach sediment.
Formation & geological history
Probably a weathered and transported clast derived from quartz-rich sandstone or metamorphosed sandstone; its exact geological age cannot be determined from the image. Rounding formed through prolonged water or sediment transport.
Uses & applications
Primarily a natural- history or lapidary specimen; quartzite can be crushed for aggregate, while attractive pieces may be polished. This ordinary pebble has little commercial value.
Geological facts
The pale patches may be quartz veins, feldspar, or weathered cement rather than a distinct gemstone. A glass-scratch test can help distinguish quartz-rich material from softer rocks.
Field identification & locations
Common in stream gravels, beaches, glacial deposits, and weathered bedrock. Test a fresh edge for quartz hardness, inspect for interlocking grains, and use dilute acid only if carbonate material is suspected.
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