Rock Identifier
Weathered sandstone or graywacke fragment (Clastic sedimentary rock, likely quartz–feldspar sandstone (exact identification requires testing)) — sedimentary
sedimentary

Weathered sandstone or graywacke fragment

Clastic sedimentary rock, likely quartz–feldspar sandstone (exact identification requires testing)

AI-generated identification · may be incorrect

Brown-gray, dull to faintly granular, with weakly visible sedimentary layering and an earthy texture; likely Mohs hardness 6–7 for quartz-rich grains, with no obvious cleavage. Specific gravity is approximately 2.4–2.7.

Identified More sedimentary
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Physical properties

Brown-gray, dull to faintly granular, with weakly visible sedimentary layering and an earthy texture; likely Mohs hardness 6–7 for quartz-rich grains, with no obvious cleavage. Specific gravity is approximately 2.4–2.7.

Formation & geological history

Formed when sand-sized mineral and rock fragments were compacted and cemented, commonly by silica, carbonate, or iron oxides; age and depositional environment cannot be determined from the photograph.

Uses & applications

Common sandstone is used for building stone, paving, aggregate, and architectural facing; this irregular specimen has mainly educational or modest collecting value.

Geological facts

The dark, weathered surface and apparent fine layering could also fit graywacke or another lithic sandstone. A fresh broken surface and acid, hardness, and grain-size tests would improve identification.

Field identification & locations

Look for visible sand grains, bedding, and gritty texture; quartz-rich sandstone scratches glass, while carbonate-cemented varieties may fizz weakly in dilute hydrochloric acid. Sandstones occur widely in sedimentary basins worldwide.