sedimentary

Sandstone Concretion

Arenaceous concretion (primarily SiO2 with Fe2O3 staining)

AI-generated identification · may be incorrect

Hardness: 6-7 (Mohs); Color: Reddish-brown, terracotta; Luster: Dull/Earthy; Structure: Clastic, botryoidal-like tuberous form; Cleavage: None

Hardness: 6-7 (Mohs)
Color: Reddish-brown, terracotta
Luster: Dull/Earthy

Identified April 13, 2026More sedimentary →

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Physical properties

Hardness: 6-7 (Mohs); Color: Reddish-brown, terracotta; Luster: Dull/Earthy; Structure: Clastic, botryoidal-like tuberous form; Cleavage: None

Formation & geological history

Formed by the precipitation of mineral cement (likely iron oxide or silica) within the spaces between sediment grains, often around a nucleus. They typically form in sedimentary basins during diagenesis.

Uses & applications

Used primarily as decorative garden stones, architectural accents, or as study specimens for geological education. Redder varieties are sometimes ground for natural pigments.

Geological facts

Concretions are often mistaken for fossils or meteorites due to their unusual, organic-looking shapes. Some can grow to several meters in diameter, such as the Moeraki Boulders in New Zealand.

Field identification & locations

Identify by its bulbous, 'tuber' shape and gritty texture. It will be harder than the surrounding host rock. Commonly found in eroded sandstone bluffs or riverbeds in arid regions like the American Southwest.