
sedimentary
Sandstone
Sedimentary Clastic Rock (Quartz Arenite)
AI-generated identification · may be incorrectHardness on Mohs scale: 6 to 7 for quartz-rich varieties; Color ranges from tan, brown, yellow, red, gray, to pink; Luster is typically dull or earthy; Crystal structure is clastic with mineral grains bound by a matrix; Cleavage is absent; Specific gravity is approximately 2.2 to 2.8.
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Physical properties
Hardness on Mohs scale: 6 to 7 for quartz-rich varieties; Color ranges from tan, brown, yellow, red, gray, to pink; Luster is typically dull or earthy; Crystal structure is clastic with mineral grains bound by a matrix; Cleavage is absent; Specific gravity is approximately 2.2 to 2.8.
Formation & geological history
Formed by the accumulation, compaction, and cementation of mineral particles or rock fragments, principally quartz and feldspar, usually deposited by water, wind, or ice in environments such as deserts, rivers, and beaches over millions of years.
Uses & applications
Widely used in construction as building stone, paving material, and flagstones; historically used for making grindstones and monuments.
Geological facts
Sandstone formations can be porous and permeable, making them excellent aquifers for storing groundwater and natural reservoirs for oil and natural gas.
Field identification & locations
Easily identified in the field by its visible grainy texture like sandpaper and distinct bedding layers; common worldwide, particularly in arid regions and ancient river basins.
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