
metamorphic
Weathered gneiss or granite fragment
Feldspar–quartz–mica rock; likely granitoid-derived gneiss
AI-generated identification · may be incorrectTan, granular, and irregular with a dull to weakly vitreous luster; visible grains suggest quartz and feldspar with minor mica. Approximate hardness 6–7 Mohs; no obvious cleavage or crystal faces are visible.
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Physical properties
Tan, granular, and irregular with a dull to weakly vitreous luster; visible grains suggest quartz and feldspar with minor mica. Approximate hardness 6–7 Mohs; no obvious cleavage or crystal faces are visible.
Formation & geological history
Likely a natural fragment weathered from granitic or gneissic bedrock, though the image alone cannot establish its exact identity or age. Such rocks commonly formed deep in the crust during Precambrian to Phanerozoic geological events.
Uses & applications
Common granite/gneiss is used as crushed aggregate, road material, building stone, and landscape rock; this small fragment has negligible commercial value.
Geological facts
The specimen appears embedded in or lying on a paved surface beside soil, and its brown color may reflect iron-oxide weathering or surface staining rather than its original composition.
Field identification & locations
Look for interlocking quartz, feldspar, and mica grains; gneiss usually shows compositional banding, while granite is more uniformly granular. Common worldwide; an isolated fragment is typically worth $0–$5.
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