
sedimentary
Weathered iron-rich sandstone or laterite
Ferruginous sandstone; predominantly quartz (SiO₂) cemented by iron oxides/hydroxides
AI-generated identification · may be incorrectBrown-orange, earthy to dull luster, fine-grained and irregularly weathered; quartz hardness 7, but the porous aggregate is friable. No obvious cleavage or crystal faces; likely low-to-moderate density.
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Physical properties
Brown-orange, earthy to dull luster, fine-grained and irregularly weathered; quartz hardness 7, but the porous aggregate is friable. No obvious cleavage or crystal faces; likely low-to-moderate density.
Formation & geological history
Formed from sand or soil enriched and cemented by hematite, goethite, and limonite during prolonged weathering and oxidation, commonly in continental or tropical settings. Exact age cannot be determined from the photograph.
Uses & applications
Usually a study or display specimen; ferruginous sandstone may be used locally as building or paving stone, while laterite is used in construction and road material.
Geological facts
The orange-brown color reflects oxidized iron rather than copper. A reddish-brown streak and magnetic response, if present, can help distinguish iron-rich material from ordinary sandstone.
Field identification & locations
Common in weathered terrains, deserts, and tropical regions. Look for visible sand grains, porous texture, earthy fracture, and orange-red coatings; dilute hydrochloric acid should produce little or no fizz.
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