Rock Identifier
Sandstone (Pebble) (Sandstone (arenite, arkose, wacke depending on composition)) — sedimentary
sedimentary

Sandstone (Pebble)

Sandstone (arenite, arkose, wacke depending on composition)

Hardness: 6-7 (Mohs), Color: Typically light brown, tan, off-white; can vary depending on mineral impurities, Luster: Dull to earthy, Crystal structure: Not applicable (rock composed of detrital grains), Cleavage: None (due to granular structure), Specific gravity: 2.6-2.7

Hardness
6-7 (Mohs), Color: Typically light brown, tan, off-white
Color
Typically light brown, tan, off-white
Identified More sedimentary

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Physical properties

Hardness: 6-7 (Mohs), Color: Typically light brown, tan, off-white; can vary depending on mineral impurities, Luster: Dull to earthy, Crystal structure: Not applicable (rock composed of detrital grains), Cleavage: None (due to granular structure), Specific gravity: 2.6-2.7

Formation & geological history

Sandstone forms from the lithification of sand, which is primarily composed of quartz grains. These grains are transported by water or wind and deposited in layers in environments such as beaches, riverbeds, deserts, and offshore bars. Over time, compaction from overlying sediments and cementation by minerals like silica (quartz), calcite, or iron oxides bind the sand grains together into solid rock. Geological age varies greatly, from Precambrian to Cenozoic, depending on the specific depositional environment.

Uses & applications

Sandstone is extensively used as a building material for facades, pavers, and ornamental applications. Due to its porous nature, it can also act as a reservoir rock for oil and natural gas. Some varieties are used as abrasives or for manufacturing glass (if high in quartz). Larger, well-rounded pebbles of sandstone, like the one shown, often indicate a history of significant transport and erosion.

Geological facts

Sandstone is one of the most common sedimentary rocks and is widely used as a building material. Its resistance to weathering makes it popular for outdoor structures. Many famous landmarks and natural formations, such as those in Zion National Park and Petra, are made of sandstone.

Field identification & locations

To identify sandstone in the field, look for a granular texture, where individual sand grains are visible and feel rough to the touch. It is typically light-colored but can be reddish, brown, or yellowish due to iron oxides. It often shows bedding planes, layers formed during deposition. The rounded shape of the specimen indicates it has been abraded and transported by water (e.g., in a river or on a beach). Common locations include riverbeds, coastlines, deserts, and areas with ancient sedimentary rock exposures. Collectors often look for unique colors, patterns, or fossils within sandstone.