Rock Identifier
Reddish-brown rock fragment, likely iron-oxide-stained sandstone (Probable quartz-rich sandstone (SiO₂ grains cemented by silica, iron oxides, or other minerals); exact identification is uncertain from the image) — sedimentary
sedimentary

Reddish-brown rock fragment, likely iron-oxide-stained sandstone

Probable quartz-rich sandstone (SiO₂ grains cemented by silica, iron oxides, or other minerals); exact identification is uncertain from the image

AI-generated identification · may be incorrect

Rough, granular surface with reddish-brown coloration, likely from iron-oxide staining; sandstone hardness varies, typically around 6–7 for quartz grains, and it has no consistent crystal cleavage. Luster appears dull; grain size and specific gravity cannot be determined reliably from the photo.

Identified More sedimentary →
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Physical properties

Rough, granular surface with reddish-brown coloration, likely from iron-oxide staining; sandstone hardness varies, typically around 6–7 for quartz grains, and it has no consistent crystal cleavage. Luster appears dull; grain size and specific gravity cannot be determined reliably from the photo.

Formation & geological history

Sandstone forms when deposited sand is compacted and cemented, across many geological ages and environments. The reddish tint commonly develops from iron oxides during or after formation.

Uses & applications

Sandstone is used as building and paving stone, dimension stone, and aggregate; this small fragment has mainly educational or collecting value.

Geological facts

The image does not provide enough detail to confirm sandstone or determine its age. A magnified view may reveal distinct sand-sized grains and cement.

Field identification & locations

Check whether grains are visible and gritty, and whether the piece scratches glass; these clues can support a quartz-rich sandstone identification. Sandstone occurs worldwide in sedimentary basins.