
sedimentary
Weathered iron-rich sandstone or ferruginous chert
Likely quartz-rich sandstone (SiO₂) cemented or stained by iron oxides such as goethite/hematite
AI-generated identification · may be incorrectBrown-orange, dull to earthy luster, fine-grained and strongly weathered, with irregular fractures and possible iron-oxide veining. Estimated hardness is about 6–7 if chert-rich, or 4–6 if sandstone; exact identification requires a scratch and acid test.
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Physical properties
Brown-orange, dull to earthy luster, fine-grained and strongly weathered, with irregular fractures and possible iron-oxide veining. Estimated hardness is about 6–7 if chert-rich, or 4–6 if sandstone; exact identification requires a scratch and acid test.
Formation & geological history
Formed from compacted quartz-rich sediment later cemented by silica and/or iron oxides, likely in a terrestrial or shallow-marine environment; age cannot be determined from the photograph.
Uses & applications
Usually a common field specimen with little commercial value; similar ferruginous sandstone is used as building or paving stone, while dense chert may be used for aggregate and historically for tools.
Geological facts
The orange-brown coloration is characteristic of oxidized iron minerals, commonly goethite and hematite. The apparent breccia-like cracks may reflect weathering, cement failure, or natural fracturing.
Field identification & locations
Look for gritty sand grains to confirm sandstone, a glassy waxy fracture and inability to scratch with a steel knife to suggest chert, and no fizz with dilute hydrochloric acid. Common worldwide in iron-rich sedimentary terrains.
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