
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 incorrectHardness 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.
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