
sedimentary
Weathered sandstone (probable quartz arenite)
Clastic sandstone, chiefly quartz (SiO₂) grains with possible feldspar and iron-oxide/calcite cement
AI-generated identification · may be incorrectTypically Mohs 6–7 for quartz grains, but friable overall; tan to cream, dull earthy luster, granular texture, and no obvious cleavage. The specimen shows weathered surfaces and faint layering or cement variation.
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Physical properties
Typically Mohs 6–7 for quartz grains, but friable overall; tan to cream, dull earthy luster, granular texture, and no obvious cleavage. The specimen shows weathered surfaces and faint layering or cement variation.
Formation & geological history
Formed when sand accumulated, was compacted, and cemented in a river, beach, dune, or shallow-marine environment; its precise geological age cannot be determined from the image. Weathering has rounded edges and exposed contrasting cement or bedding.
Uses & applications
Used as building stone, paving, aggregate, and ornamental stone; attractive varieties are cut for slabs and landscaping. Ordinary hand specimens generally have little commercial value.
Geological facts
Sandstone commonly preserves cross-bedding, ripple marks, mud cracks, and fossils, making it important for reconstructing ancient environments. Iron oxides produce the common tan, yellow, red, and brown colors.
Field identification & locations
Look for visible sand grains, gritty texture, bedding, and acid-insensitive quartz-rich composition; a hand lens and streak/acid tests help distinguish it from limestone. Common worldwide, especially in sedimentary basins and desert, coastal, and river deposits.
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