Rock Identifier
Iron-rich sandstone or weathered lateritic rock (Ferruginous sandstone; chiefly quartz (SiO₂) with iron oxides/hydroxides such as hematite and goethite) — sedimentary
sedimentary

Iron-rich sandstone or weathered lateritic rock

Ferruginous sandstone; chiefly quartz (SiO₂) with iron oxides/hydroxides such as hematite and goethite

AI-generated identification · may be incorrect

Hardness commonly 5–7 Mohs; tan to reddish-brown, earthy to dull/satin luster, fine-grained and apparently massive, with no obvious cleavage. The specimen appears porous and weathered, but exact identification from a photograph is limited.

Identified More sedimentary
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Physical properties

Hardness commonly 5–7 Mohs; tan to reddish-brown, earthy to dull/satin luster, fine-grained and apparently massive, with no obvious cleavage. The specimen appears porous and weathered, but exact identification from a photograph is limited.

Formation & geological history

Forms when quartz-rich sand is cemented by silica and iron minerals, often in oxidizing terrestrial environments; lateritic pieces develop through intense tropical weathering. The geological age cannot be determined visually and may range from relatively young to ancient.

Uses & applications

Used locally as building or landscaping stone and as a source rock in some iron-rich deposits; attractive pieces may be collected, but this small rough fragment has little commercial value.

Geological facts

The rusty coloration comes from oxidized iron rather than necessarily indicating metallic iron. A streak, hardness, and acid test would distinguish it from iron-rich limestone or slag.

Field identification & locations

Look for gritty sand-sized grains, earthy red-brown coloration, and a white-to-reddish streak; quartz grains should resist scratching by a steel knife. Common in arid and tropical weathering zones worldwide; test magnetism and inspect with a loupe for slag-like glassiness.