
sedimentary
Sandstone
Quartz-rich clastic sedimentary rock, commonly arkose or lithic sandstone
AI-generated identification · may be incorrectTypically Mohs hardness 6–7 for quartz-rich grains, tan to orange color, dull to slightly gritty luster, and visible sand-sized grains cemented together; composition appears dominated by quartz with possible feldspar, iron-oxide staining, and clay minerals.…
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Physical properties
Typically Mohs hardness 6–7 for quartz-rich grains, tan to orange color, dull to slightly gritty luster, and visible sand-sized grains cemented together; composition appears dominated by quartz with possible feldspar, iron-oxide staining, and clay minerals. Usually porous, with no consistent cleavage and irregular fracture.
Formation & geological history
Formed when sand accumulated, compacted, and cemented—often by silica, calcite, or iron oxides—in rivers, dunes, beaches, or shallow marine settings. Its exact geological age cannot be determined from the image and may range from Precambrian to recent.
Uses & applications
Used as building stone, paving, aggregate, landscaping material, and occasionally as a sculptural or decorative stone. This ordinary field specimen generally has little commercial or collector value.
Geological facts
The orange-brown coloration commonly results from hematite or limonite coatings on grains or cement. Sandstone can preserve ripple marks, cross-bedding, fossils, and ancient environmental clues.
Field identification & locations
Identify it by its gritty texture, sand-sized grains, layered or massive appearance, and tendency to shed grains when weathered; a glass scratch test may help if quartz-rich. Common worldwide, especially in sedimentary basins and desert or river deposits.
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