sedimentary

Conglomerate

Conglomerate (clastic sedimentary rock)

AI-generated identification · may be incorrect

Hardness: variable (depends on clast type, matrix usually 3-7 Mohs); Color: tan, brown, or grey matrix with multi-colored rounded clasts; Luster: dull/earthy matrix; Crystal structure: none (clastic texture); Cleavage: none; Specific gravity: 2.3–2.8

Hardness: variable (depends on clast type, matrix usually 3-7 Mohs)
Color: tan, brown, or grey matrix with multi-colored rounded clasts
Luster: dull/earthy matrix

Identified April 25, 2026More sedimentary →

Explore Conglomerate in the encyclopedia →

Identify your own rocks.

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

App Store Google Play

Physical properties

Formation & geological history

Formed in high-energy environments like fast-moving rivers, alluvial fans, or beaches where water is strong enough to transport large, rounded pebbles. These sediment grains are later buried and cemented together by minerals like calcite or quartz over millions of years.

Uses & applications

Used primarily in the construction industry as coarse aggregate for concrete, as fill material for road beds, and occasionally as decorative dimension stone if the colors are unique.

Geological facts

Conglomerate is often called 'puddingstone' because the rounded pebbles look like raisins in a pudding. It is one of the few rocks that tells a story of an ancient high-velocity water source, such as a prehistoric riverbed.

Field identification & locations

Identify in the field by looking for rounded pebbles (clasts) larger than 2mm that are firmly 'glued' into a finer matrix. Unlike breccia, the pieces in conglomerate are rounded, indicating they traveled long distances in water. Commonly found in river basins and ancient mountain margins.