
sedimentary
Weathered sandstone
Quartz-rich sandstone, commonly arkose or lithic sandstone
AI-generated identification · may be incorrectTypically Mohs hardness 6–7 because of quartz; the specimen appears pinkish-brown, granular, dull to slightly earthy, and lacks obvious cleavage. Sand grains are cemented together, likely by silica, iron oxides, or calcite.
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Physical properties
Typically Mohs hardness 6–7 because of quartz; the specimen appears pinkish-brown, granular, dull to slightly earthy, and lacks obvious cleavage. Sand grains are cemented together, likely by silica, iron oxides, or calcite.
Formation & geological history
Formed when sand accumulated in rivers, beaches, dunes, or shallow marine settings and lithified through compaction and cementation. Its exact geological age cannot be determined from the image; sandstone ranges from Precambrian to modern formations.
Uses & applications
Used as building stone, paving, wall material, aggregate, and occasionally sculpture stone; attractive varieties are collected or used decoratively. This ordinary piece has minimal commercial value.
Geological facts
The pink coloration commonly reflects feldspar or iron-oxide staining, while visible grains indicate clastic sedimentary origin. Weathering rounds edges and can loosen surface grains.
Field identification & locations
Identify sandstone by its gritty texture, visible sand-sized grains, layered or speckled appearance, and possible weak scratching of glass; acid reaction suggests calcite cement. Common worldwide, especially in sedimentary basins and river gravels.
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