
sedimentary
Weathered iron-rich sandstone or laterite
Ferruginous sandstone; chiefly quartz (SiO₂) cemented or stained by iron oxides such as hematite and goethite
AI-generated identification · may be incorrectBrown to rusty-red, dull to earthy luster, visibly granular and porous, with no obvious crystals or cleavage. Typically Mohs hardness 6–7 for quartz grains but friable overall; specific gravity commonly about 2.3–2.7.
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Physical properties
Brown to rusty-red, dull to earthy luster, visibly granular and porous, with no obvious crystals or cleavage. Typically Mohs hardness 6–7 for quartz grains but friable overall; specific gravity commonly about 2.3–2.7.
Formation & geological history
Likely formed from sand-sized quartz grains lithified and later impregnated by oxidized iron during weathering; alternatively it may be a lateritic ironstone. Exact age and locality cannot be determined from the photograph.
Uses & applications
Used locally as building stone, road aggregate, and iron-rich raw material; attractive pieces may be collected as natural specimens. It has little jewelry value unless polished and unusually patterned.
Geological facts
The rusty coloration reflects iron oxidation, similar to the process that produces rust on steel. A dark streak or strongly magnetic response would suggest abundant magnetite or hematite, while fizzing in dilute acid would indicate carbonate cement.
Field identification & locations
Identify by its gritty texture, uneven weathered surface, and reddish-brown iron staining; test with a steel nail, streak plate, magnet, and dilute hydrochloric acid. Common in arid, tropical, and strongly weathered sedimentary terrains.
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