
sedimentary
Likely iron-rich sandstone or weathered hematite-bearing rock
Quartz-rich sandstone, possibly ferruginous sandstone (SiO₂ with iron oxides such as hematite/goethite)
AI-generated identification · may be incorrectBrown-red, dull to earthy luster, visibly granular and fine-grained, with uneven fracture and no obvious cleavage. Likely Mohs hardness about 5–7, though loose grains may scratch more easily; specific gravity is variable, commonly 2.3–3.0.
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Physical properties
Brown-red, dull to earthy luster, visibly granular and fine-grained, with uneven fracture and no obvious cleavage. Likely Mohs hardness about 5–7, though loose grains may scratch more easily; specific gravity is variable, commonly 2.3–3.0.
Formation & geological history
Probably formed from compacted and cemented sand, later stained or cemented by iron oxides during weathering. Its precise geological age cannot be determined from the photograph.
Uses & applications
Common sandstone is used for building stone, paving, aggregate, and decorative pieces; iron-rich varieties are mainly collected as geological specimens. It has little jewelry value unless unusually attractive or polished.
Geological facts
The reddish-brown color commonly comes from microscopic hematite coating quartz grains. A streak test, hardness test, and acid test would help distinguish it from iron ore, chert, or a metamorphic rock.
Field identification & locations
Look for sand-sized quartz grains and rusty cement; quartz-rich pieces should scratch glass, while hematite-rich material leaves a reddish-brown streak. Common worldwide, especially in arid and oxidizing sedimentary environments.
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