Rock Identifier
Weathered iron-rich sandstone or laterite fragment (Ferruginous sandstone, chiefly quartz (SiO₂) cemented or stained by iron oxides/hydroxides) — sedimentary
sedimentary

Weathered iron-rich sandstone or laterite fragment

Ferruginous sandstone, chiefly quartz (SiO₂) cemented or stained by iron oxides/hydroxides

AI-generated identification · may be incorrect

Hardness about 5–7 where quartz-rich; rusty orange-brown, granular, dull to earthy luster, with irregular fracture and no obvious cleavage. The porous, rough texture and iron staining are consistent with weathered sandstone or lateritic material.

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Physical properties

Hardness about 5–7 where quartz-rich; rusty orange-brown, granular, dull to earthy luster, with irregular fracture and no obvious cleavage. The porous, rough texture and iron staining are consistent with weathered sandstone or lateritic material.

Formation & geological history

Likely formed from quartz sand lithified and later impregnated by iron oxides during oxidation and weathering; its precise geological age cannot be determined from the photograph. Common in terrestrial sedimentary basins and tropical weathering profiles.

Uses & applications

Common material has little commercial value, though ferruginous sandstone may be used locally as aggregate, building stone, or decorative landscaping rock.

Geological facts

The orange-brown coloration typically comes from hematite and goethite rather than abundant orange minerals. A magnet may show weak attraction if magnetite is present, but iron staining alone is not strongly magnetic.

Field identification & locations

Look for visible sand grains, rusty cement, pores, and streaking; it differs from solid iron ore by its granular sandstone texture. Common worldwide, especially Australia, India, Africa, and weathered continental regions.