sedimentary

Sandstone with Liesegang Rings

Arenite with Iron Oxide Concretions

AI-generated identification · may be incorrect

Hardness: 6-7 (Mohs); Color: Tan, white, and reddish-brown; Luster: Dull/Earthy; Structure: Clastic; Cleavage: None; Specific Gravity: 2.2-2.8

Hardness: 6-7 (Mohs)
Color: Tan, white, and reddish-brown
Luster: Dull/Earthy

Identified May 9, 2026More sedimentary →

Explore Sandstone with Liesegang Rings 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); Color: Tan, white, and reddish-brown; Luster: Dull/Earthy; Structure: Clastic; Cleavage: None; Specific Gravity: 2.2-2.8

Formation & geological history

Formed through the accumulation and cementation of sand-sized mineral grains or rock fragments. The circular patterns (Liesegang rings) are secondary chemical precipitates formed by the rhythmic deposition of iron oxides from groundwater.

Uses & applications

Primarily used as a decorative garden stone, building material, or as a specimen for geological study and mineral collecting.

Geological facts

The rhythmic bands, called Liesegang rings, are named after the German chemist Raphael E. Liesegang. They were first observed in chemical precipitates in gels but are commonly found in sedimentary rocks.

Field identification & locations

Identify by its gritty texture and the distinctive concentric circular or wavy bands of color. Often found in arid environments or areas with significant groundwater movement through porous rock.