
sedimentary
Sandstone
Quartzose Sandstone / Lithic Sandstone
AI-generated identification · may be incorrectHardness of 6 to 7 on the Mohs scale, colors range from tan, brown, yellow, red, to grey depending on iron oxides and impurities, dull or earthy luster, granular texture composed of quartz and feldspar grains, poor to moderate cleavage.
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Physical properties
Hardness of 6 to 7 on the Mohs scale, colors range from tan, brown, yellow, red, to grey depending on iron oxides and impurities, dull or earthy luster, granular texture composed of quartz and feldspar grains, poor to moderate cleavage.
Formation & geological history
Formed by the accumulation, compaction, and cementation of mineral particles or rock fragments, mainly quartz, deposited by water, wind, or ice in environments such as deserts, rivers, and beaches over millions of years.
Uses & applications
Widely used as a construction material for building facades, paving stones, flagstones, retaining walls, and historically for grinding stones and whetstones.
Geological facts
Sandstone formations often display prominent layers called cross-bedding, which reveal the direction of ancient winds or water currents. Famous monuments worldwide, including parts of Petra and the Great Temple of Abu Simbel, are carved directly into sandstone cliffs.
Field identification & locations
Easily identified by its gritty, sandpaper-like texture and visible mineral grains. It is commonly found globally in sedimentary basins, desert regions, and river valleys.
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