
sedimentary
Weathered sandstone or iron-stained sedimentary rock
Quartz-rich sandstone, likely ferruginous sandstone (SiO₂ with iron-oxide cement)
AI-generated identification · may be incorrectHardness about 6–7 for quartz grains; brown to ochre, dull to earthy luster, and visibly granular/porous. Individual grains appear cemented together, with no obvious cleavage or large crystals; specific gravity is typically 2.2–2.7.
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Physical properties
Hardness about 6–7 for quartz grains; brown to ochre, dull to earthy luster, and visibly granular/porous. Individual grains appear cemented together, with no obvious cleavage or large crystals; specific gravity is typically 2.2–2.7.
Formation & geological history
Formed when sand accumulated, compacted, and cemented in a sedimentary basin; the rusty color comes from oxidized iron minerals such as hematite or goethite. Its exact geological age cannot be determined from the photograph.
Uses & applications
Common sandstone is used as building stone, paving, aggregate, and landscaping material; attractive pieces may be collected or cut for decorative use, though this specimen appears ordinary.
Geological facts
Iron staining commonly produces yellow, orange, red, and brown tones in sandstone. Surface weathering can make the rock look darker and rougher than its fresh interior.
Field identification & locations
Look for visible sand grains, gritty texture, uneven fracture, and a lack of interlocking crystals; a steel nail generally will not scratch quartz-rich sandstone, but the cement may vary. Sandstone occurs widely in former beaches, deserts, river channels, and sedimentary plateaus worldwide.
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