Rock Identifier
Weathered sandstone or iron-stained sedimentary rock (Likely quartz-rich sandstone (SiO₂) with iron-oxide staining; exact identification requires testing) — sedimentary
sedimentary

Weathered sandstone or iron-stained sedimentary rock

Likely quartz-rich sandstone (SiO₂) with iron-oxide staining; exact identification requires testing

AI-generated identification · may be incorrect

Tan to ochre, dull earthy luster, visibly granular and porous with irregular weathering. Likely Mohs hardness about 6–7 for quartz grains, but weak cement may crumble; no obvious cleavage or crystals are visible.

Identified More sedimentary
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Physical properties

Tan to ochre, dull earthy luster, visibly granular and porous with irregular weathering. Likely Mohs hardness about 6–7 for quartz grains, but weak cement may crumble; no obvious cleavage or crystals are visible.

Formation & geological history

Probably lithified sand cemented by silica, calcite, or iron oxides, then exposed and weathered at the surface; age cannot be determined from the photograph. Its rough texture and rusty color suggest oxidation of iron-bearing minerals.

Uses & applications

Common sandstone is used as building stone, paving, aggregate, and decorative rock; this small specimen has mainly educational or collectible value.

Geological facts

Iron oxides such as hematite and goethite commonly produce yellow, orange, and reddish-brown sandstone coloration. The apparent granular texture distinguishes it from most massive igneous rocks.

Field identification & locations

Look for sand-sized quartz grains, layered bedding, and a gritty feel; a hand lens and dilute hydrochloric acid can help detect carbonate cement. Common worldwide in former beaches, dunes, river channels, and deserts.