Sedimentary rock

Sandstone

Arenite (a specific type of sandstone with less than 15% matrix)

Identified August 28, 2025More sedimentary rock →

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Physical properties

Hardness varies depending on cementation and grain composition, typically 6-7 on Mohs scale (for quartz grains). Color is commonly reddish-brown due to iron oxides, but can also be yellowish, grayish, or white. Luster is dull to earthy. Crystal structure is not applicable as it's a clastic sedimentary rock; it's composed of individual mineral grains (often sub-angular to rounded quartz) cemented together. No distinct cleavage. Specific gravity is typically 2.65-2.70.

Formation & geological history

Sandstone forms from the consolidation and cementation of sand grains. These grains are typically deposited in environments where sand accumulates, such as deserts (forming dunes), beaches, riverbeds, and deltaic environments. Over time, as more layers of sediment accumulate above, the sand grains are compacted, and groundwater flowing through the pores deposits minerals like silica, calcium carbonate, or iron oxides, which act as cement, binding the grains together. The geological age of sandstone varies widely, from Precambrian to recent, depending on the specific formation.

Uses & applications

Sandstone is widely used as a building material for construction (facades, paving, decorative elements), in abrasive applications (grinding stones), and as a source of silica for glass manufacturing. It has also been used in some instances for carving and statuary due to its relatively even texture.

Geological facts

Sandstone has been used as a building material for centuries, with many famous structures like the Egyptian pyramids and parts of the Roman Colosseum incorporating it. The color of sandstone is often indicative of the minerals present, particularly iron oxides for reds and yellows.

Field identification & locations

In the field, sandstone can be identified by its gritty feel, as it is composed of sand-sized grains. Running a fingernail across it will often dislodge small grains. The specific rock in the image appears to be a well-rounded piece of reddish sandstone, likely from a fluvial (river) or beach environment where it has undergone significant abrasion. It's commonly found in sedimentary basins worldwide. Tips for collectors include looking for distinct bedding planes, cross-bedding (indicating ancient dune or ripple formations), and fossil remnants within the rock.

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Sedimentary rock with quartz veining

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Quartz Vein in Sedimentary Rock

Silicon Dioxide (SiO2) with host Chert or Limestone

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