Rock Identifier
Sandstone (Sedimentary Clastic Rock (Quartz Arenite)) — sedimentary
sedimentary

Sandstone

Sedimentary Clastic Rock (Quartz Arenite)

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.

Identified More sedimentary
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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.