Rock Identifier
Weathered iron-rich sandstone or laterite fragment (Ferruginous sandstone, likely hematite/goethite-cemented sandstone (exact identification requires testing)) — sedimentary
sedimentary

Weathered iron-rich sandstone or laterite fragment

Ferruginous sandstone, likely hematite/goethite-cemented sandstone (exact identification requires testing)

AI-generated identification · may be incorrect

Hardness typically 5–7, rusty red-brown with gray patches, dull to earthy luster, fine-grained and massive; iron staining and a prominent fracture are visible. It may feel moderately heavy, but no diagnostic crystal cleavage is apparent.

Identified More sedimentary
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Physical properties

Hardness typically 5–7, rusty red-brown with gray patches, dull to earthy luster, fine-grained and massive; iron staining and a prominent fracture are visible. It may feel moderately heavy, but no diagnostic crystal cleavage is apparent.

Formation & geological history

Likely formed when quartz-rich sand was cemented by iron oxides, or when iron-rich soil/laterite hardened during intense weathering. Its age cannot be determined from the photograph; such materials occur from Precambrian to recent deposits.

Uses & applications

Commonly used as low-grade building or landscaping stone and occasionally as an iron-ore material if iron content is high. This ordinary weathered fragment has little jewelry value.

Geological facts

The red coloration commonly comes from hematite and the yellow-brown tones from goethite or limonite. A dark red streak, magnetism, and density tests can help distinguish ferruginous sandstone from ordinary sandstone.

Field identification & locations

Common in arid, tropical, and strongly weathered terrains, including Australia, India, Africa, and the Americas. Check streak on unglazed porcelain, hardness against steel/glass, and texture with a hand lens; acid reaction should be absent.