sedimentary

Concretion (Sandstone)

Carbonate-cemented Sandstone Concretion

AI-generated identification · may be incorrect

Hardness: 3-5 (Mohs scale), Color: tan/beige to grey with dark specks, Luster: dull/earthy, Crystal structure: microcrystalline cement, Cleavage: none (fractures irregularly)

Identified April 29, 2026More sedimentary →

Explore Concretion (Sandstone) in the encyclopedia →

Identify your own rocks.

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

App Store Google Play

Physical properties

Hardness: 3-5 (Mohs scale), Color: tan/beige to grey with dark specks, Luster: dull/earthy, Crystal structure: microcrystalline cement, Cleavage: none (fractures irregularly)

Formation & geological history

Formed through the precipitation of mineral cement (typically calcite or iron oxides) in the spaces between sediment grains, often around a nucleus like a leaf or shell. This occurs within sedimentary layers before they are fully deeply buried.

Uses & applications

Primarily used as decorative display pieces, geological curiosities, or for educational purposes. Large ones are used in landscaping.

Geological facts

Concretions are often mistaken for fossilized eggs, dinosaur bones, or even man-made artifacts like cannonballs due to their perfectly spherical shape.

Field identification & locations

Identify by their rounded, often spherical or disc-like shape that differs from the surrounding rock. Common in sandstone or shale formations. Look for a 'seed' or nucleus in the center if cracked open.