Rock Identifier
Sandstone (Sandstone (composed predominantly of Quartz, SiO2, with Feldspar and Clay minerals)) — sedimentary
sedimentary

Sandstone

Sandstone (composed predominantly of Quartz, SiO2, with Feldspar and Clay minerals)

Hardness: 6-7 (varies based on cementation); Color: Yellowish-brown, tan, reddish-brown, green tint from lichen/weathering; Luster: Dull, earthy; Crystal structure: Granular, clastic texture; Cleavage: None; Specific Gravity: 2.2-2.8

Hardness
6-7 (varies based on cementation)
Luster
Dull, earthy
Identified More sedimentary
Explore Sandstone in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Hardness: 6-7 (varies based on cementation); Color: Yellowish-brown, tan, reddish-brown, green tint from lichen/weathering; Luster: Dull, earthy; Crystal structure: Granular, clastic texture; Cleavage: None; Specific Gravity: 2.2-2.8

Formation & geological history

Formed by the compaction and cementation of mineral particles or rock fragments, usually quartz and feldspar, deposited in desert, river, beach, or shallow sea environments over millions of years.

Uses & applications

Widely used as a construction material, paving stone, decorative landscaping stone, and historically for grindstones and sculpture. Important reservoir rock for groundwater and petroleum.

Geological facts

Sandstone accounts for roughly 20 to 25 percent of all sedimentary rocks. Famous landmarks made of sandstone include Petra in Jordan and the Grand Canyon strata in the USA.

Field identification & locations

Identified in the field by its distinctive gritty feel, coarse sand-sized grains, and often visible layering or bedding planes. Very common globally in sedimentary basins, riverbeds, and cliffs.