
sedimentary
Weathered sandstone
Quartz-rich sandstone, likely arkose or feldspathic sandstone
AI-generated identification · may be incorrectTan to brown, fine- to medium-grained, granular texture with visible quartz/feldspar and iron-oxide staining; typically Mohs 6–7 for grains but weakly cemented overall, earthy to dull luster, no cleavage, porous, and commonly bedded.
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Physical properties
Tan to brown, fine- to medium-grained, granular texture with visible quartz/feldspar and iron-oxide staining; typically Mohs 6–7 for grains but weakly cemented overall, earthy to dull luster, no cleavage, porous, and commonly bedded.
Formation & geological history
Formed when sand accumulated in rivers, beaches, dunes, or alluvial fans and lithified by compaction and silica, calcite, or iron-oxide cement. Its exact age cannot be determined from the image; sandstone ranges from Precambrian to modern geologic formations.
Uses & applications
Used as building stone, paving, aggregate, and decorative landscaping material; attractive slabs may be used ornamentally, though this specimen appears mainly a common field rock.
Geological facts
The rusty coloration generally reflects oxidized iron minerals, while the pale grains are probably quartz and feldspar. Weathering has rounded and weakened the exposed surfaces.
Field identification & locations
Identify it by gritty sand-sized grains, layered or massive sedimentary fabric, and ability to scratch glass if quartz-rich; dilute acid may fizz only if carbonate cement is present. Common worldwide, especially in sedimentary basins and desert or river environments.
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