Rock Identifier
Sandstone (Clastic sedimentary rock (Quartz arenite / Arkose)) — sedimentary
sedimentary

Sandstone

Clastic sedimentary rock (Quartz arenite / Arkose)

Hardness: 6-7 (due to quartz grains); Color: Varies from brown, red, tan, yellow to grey; Luster: Dull to earthy; Structure: Clastic, granular texture composed of cemented mineral particles or rock fragments; Cleavage: None (fractures irregularly); Specific Gravity: 2.2-2.8

Hardness
6-7 (due to quartz grains)
Color
Varies from brown, red, tan, yellow to grey
Luster
Dull to earthy
Identified More sedimentary
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Physical properties

Hardness: 6-7 (due to quartz grains); Color: Varies from brown, red, tan, yellow to grey; Luster: Dull to earthy; Structure: Clastic, granular texture composed of cemented mineral particles or rock fragments; Cleavage: None (fractures irregularly); Specific Gravity: 2.2-2.8

Formation & geological history

Formed by the accumulation, compaction, and cementation of mineral particles or rock fragments, chiefly quartz and feldspar, typically 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 buildings, paving, and decorative stonework, as well as an aggregate in road construction.

Geological facts

Sandstone is porous and permeable, making it an excellent natural aquifer that stores and filters groundwater. Many famous ancient monuments, such as Petra in Jordan and the temples of Angkor Wat, are carved directly out of sandstone formations.

Field identification & locations

Easily identified by its gritty, sandpaper-like texture and visible mineral grains. It is commonly found in sedimentary basins worldwide, particularly in arid regions and ancient riverbeds.