Rock Identifier
Weathered sandstone or mudstone (Clastic siliciclastic sedimentary rock, probably quartz-rich sandstone; exact identification requires a fresh surface and tests) — sedimentary
sedimentary

Weathered sandstone or mudstone

Clastic siliciclastic sedimentary rock, probably quartz-rich sandstone; exact identification requires a fresh surface and tests

AI-generated identification · may be incorrect

Tan-yellow, dull and fine to medium grained, with iron-oxide staining and weak bedding/fracturing; likely Mohs hardness about 5–7 for sandstone, lower if mudstone, with no obvious cleavage and low-to-moderate density.

Identified More sedimentary
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Physical properties

Tan-yellow, dull and fine to medium grained, with iron-oxide staining and weak bedding/fracturing; likely Mohs hardness about 5–7 for sandstone, lower if mudstone, with no obvious cleavage and low-to-moderate density.

Formation & geological history

Formed when sand or silt accumulated, compacted, and cemented in an ancient river, floodplain, lake, or shallow-marine environment; its age cannot be determined from the image and may range from Paleozoic to recent.

Uses & applications

Common sandstone is used as building stone, paving, aggregate, and occasionally decorative material; ordinary hand specimens generally have minimal commercial value.

Geological facts

The rusty coloration is typically caused by hematite or limonite cement, while the rounded surface reflects weathering and abrasion.

Field identification & locations

Look for visible sand grains, layered texture, and a gritty feel; a dilute hydrochloric-acid test should show little reaction unless carbonate cement is present. Common worldwide, especially in sedimentary basins.