sedimentary

Sandstone Concretion

Clastic sedimentary rock (primarily Quartz SiO2)

AI-generated identification · may be incorrect

Hardness: 6-7 (Mohs scale); Color: tan, buff, or light brown; Luster: dull/earthy; Texture: granular, sandy feel; Crystal structure: none (clastic); Cleavage: none.

Hardness: 6-7 (Mohs scale)
Color: tan, buff, or light brown
Luster: dull/earthy

Identified April 25, 2026More sedimentary →

Explore Sandstone Concretion in the encyclopedia →

Identify your own rocks.

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

App Store Google Play

Physical properties

Hardness: 6-7 (Mohs scale); Color: tan, buff, or light brown; Luster: dull/earthy; Texture: granular, sandy feel; Crystal structure: none (clastic); Cleavage: none.

Formation & geological history

Formed by the precipitation of mineral cement (like calcite or silica) within the spaces between sand grains. This often happens around a nucleus, such as a fossil or organic matter, during the diagenesis process in sedimentary basins over millions of years.

Uses & applications

Commonly collected as curiosities due to their strange shapes. Sandstone generally is used in construction and paving, though concretions specifically are used for landscaping or as decorative objects.

Geological facts

Concretions are often mistaken for fossils, eggs, or man-made tools due to their unusual and sometimes ergonomic shapes. Some giant concretions, like the Moeraki Boulders in New Zealand, can grow to several meters in diameter.

Field identification & locations

Identify by the sandy texture and often rounded or bulbous shapes that stand out from the surrounding flatter layers of rock. Found in sandstone outcrops, riverbeds, and desert regions where erosion exposes them.