sedimentary

Banded Sandstone (Wonderstone)

Sandstone with Liesegang Rings (SiO2 with Iron Oxides)

Hardness: 6-7 (Mohs scale); Color: Tan, brown, ochre, and grey; Luster: Dull/Earthy; Crystal structure: Granular/Clastic; Cleavage: None/Conchoidal. It has a rough texture but can be smooth when water-worn.

Hardness: 6-7 (Mohs scale)
Color: Tan, brown, ochre, and grey
Luster: Dull/Earthy

Identified April 26, 2026More sedimentary →

Identify your own rocks.

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

App Store Google Play

Physical properties

Formation & geological history

Formed through the accumulation and cementation of mineral particles (sand). The banding, known as Liesegang rings, is formed by the chemical precipitation of iron oxides (hematite or limonite) from groundwater moving through the porous rock.

Uses & applications

Used primarily for decorative purposes in landscaping, garden accents, and small lapidary crafts (cabochons). Historically used as building material where abundant.

Geological facts

The distinct banding often mimics wood grain or topographical maps. These rings form through a phenomenon of rhythmic precipitation in a fluid-saturated porous medium, occurring long after the rock itself was deposited.

Field identification & locations

Identify by its gritty texture and characteristic concentric, rhythmic color bands that follow a different pattern than the original sedimentary bedding. Commonly found in arid regions, riverbeds, and sandstone canyons like those in the American Southwest.

Other sedimentary specimens

See all

Sandstone or Siltstone

Arenite (if sandstone)

Sedimentary

Chert Breccia

Brecciated Chert (Microcrystalline Silica)

sedimentary

Sandstone Grain

Clastic Sedimentary Rock Grain (SiO2 dominated)

sedimentary

Sandstone

Arenite (primarily SiO2)

sedimentary

Shale or Slaty Mudstone

Argillaceous sedimentary rock

sedimentary

Sandstone

Arenite

sedimentary