sedimentary

Pink sandstone or weathered sedimentary stone

Likely quartz-rich sandstone (lithified siliciclastic sediment)

AI-generated identification · may be incorrect

Muted pink-tan, matte and fine-grained with irregular edges and no visible crystals; likely Mohs hardness ~6–7, depending on cement, with poor cleavage and specific gravity about 2.2–2.7. The smooth appearance may reflect polishing, abrasion, or coating.

Identified August 16, 2026More sedimentary →

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Physical properties

Formation & geological history

Sandstone forms when sand-sized grains—commonly quartz and feldspar—are compacted and cemented, often in ancient river, dune, or beach environments. The image alone cannot establish its geological age.

Uses & applications

Common sandstone is used for building stone, paving, landscaping, and decorative objects; attractive pieces may be sold as inexpensive specimens or craft stones.

Geological facts

The pink color commonly comes from iron-oxide coatings on quartz or feldspar grains. Fine texture and lack of obvious layering make precise identification difficult from the photograph.

Field identification & locations

Check a fresh edge with a 10× loupe for sand-sized grains and test an inconspicuous area: quartz-rich sandstone scratches glass, while calcite-rich stone fizzes weakly with dilute acid. Common worldwide, especially in sedimentary basins.