
sedimentary
Likely weathered sandstone or fine-grained granite
Quartz–feldspar-rich lithic rock; exact identification requires a fresh surface and testing
AI-generated identification · may be incorrectGray-brown, fine- to medium-grained, dull to slightly sparkly surface with apparent granular texture and irregular fracture. Likely Mohs hardness 6–7 if quartz-rich; cleavage is not evident, and specific gravity is approximately 2.5–2.7.
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Physical properties
Gray-brown, fine- to medium-grained, dull to slightly sparkly surface with apparent granular texture and irregular fracture. Likely Mohs hardness 6–7 if quartz-rich; cleavage is not evident, and specific gravity is approximately 2.5–2.7.
Formation & geological history
The specimen appears naturally weathered and broken, possibly from an exposed outcrop or geologic sampling site. If sandstone, it formed by burial and cementation of sand, generally from Paleozoic to Cenozoic strata; if granite, it crystallized slowly underground and may be much older.
Uses & applications
Sandstone is used for building stone, paving, aggregate, and decorative pieces; granite is widely used for construction, countertops, monuments, and aggregate. This small fragment has negligible commercial value.
Geological facts
The visible granular texture and subdued color are consistent with sandstone, but the image is insufficient to distinguish it confidently from weathered granite or gneiss.
Field identification & locations
Check a freshly broken face: visible interlocking quartz and feldspar crystals suggest granite, while rounded sand grains in a cemented matrix suggest sandstone. Common localities are widespread worldwide; an acid test, hand lens, streak, and hardness test would improve identification.
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