
sedimentary
Iron-rich sandstone (ferruginous sandstone)
Ferruginous sandstone, composed mainly of quartz (SiO₂) cemented by iron oxides such as hematite or goethite
AI-generated identification · may be incorrectBrown, rough, granular surface with scattered darker grains; likely Mohs hardness about 6–7, vitreous quartz grains, and no distinct cleavage. Exact composition and properties cannot be confirmed from the photo alone.
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Physical properties
Brown, rough, granular surface with scattered darker grains; likely Mohs hardness about 6–7, vitreous quartz grains, and no distinct cleavage. Exact composition and properties cannot be confirmed from the photo alone.
Formation & geological history
Forms when sand grains are deposited, buried, and cemented by iron-rich minerals; its age depends on the source formation and cannot be determined visually.
Uses & applications
Commonly used as building or landscaping stone where durable; iron-rich varieties may be collected for their color and texture.
Geological facts
Iron-oxide cement gives ferruginous sandstone its rusty brown to red coloration and can make it noticeably heavier or harder than weakly cemented sandstone.
Field identification & locations
Look for visible sand-sized grains and rusty iron staining; it should feel gritty rather than crystalline. Ferruginous sandstone occurs in sedimentary basins worldwide.
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