Rock Identifier
Weathered sandstone (probable quartz arenite) (Clastic sandstone, chiefly quartz (SiO₂) grains with possible feldspar and iron-oxide/calcite cement) — sedimentary
sedimentary

Weathered sandstone (probable quartz arenite)

Clastic sandstone, chiefly quartz (SiO₂) grains with possible feldspar and iron-oxide/calcite cement

AI-generated identification · may be incorrect

Typically Mohs 6–7 for quartz grains, but friable overall; tan to cream, dull earthy luster, granular texture, and no obvious cleavage. The specimen shows weathered surfaces and faint layering or cement variation.

Identified More sedimentary
Explore Weathered sandstone (probable quartz arenite) in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Typically Mohs 6–7 for quartz grains, but friable overall; tan to cream, dull earthy luster, granular texture, and no obvious cleavage. The specimen shows weathered surfaces and faint layering or cement variation.

Formation & geological history

Formed when sand accumulated, was compacted, and cemented in a river, beach, dune, or shallow-marine environment; its precise geological age cannot be determined from the image. Weathering has rounded edges and exposed contrasting cement or bedding.

Uses & applications

Used as building stone, paving, aggregate, and ornamental stone; attractive varieties are cut for slabs and landscaping. Ordinary hand specimens generally have little commercial value.

Geological facts

Sandstone commonly preserves cross-bedding, ripple marks, mud cracks, and fossils, making it important for reconstructing ancient environments. Iron oxides produce the common tan, yellow, red, and brown colors.

Field identification & locations

Look for visible sand grains, gritty texture, bedding, and acid-insensitive quartz-rich composition; a hand lens and streak/acid tests help distinguish it from limestone. Common worldwide, especially in sedimentary basins and desert, coastal, and river deposits.