sedimentary

Conglomerate

Conglomerate rock

Hardness: variable (depends on clast composition, typically 6-7 if quartz-rich); Color: brown, tan, yellow, orange due to iron oxide staining; Luster: dull to waxy; Structure: clastic texture with rounded rock fragments (>2mm) in a finer-grained matrix; Cleavage: none; SG: 2.6-2.8.

Color: brown, tan, yellow, orange due to iron oxide staining
Luster: dull to waxy

Identified April 27, 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 in high-energy environments like fast-moving rivers, alluvial fans, or beaches where rounded stones are deposited and later cemented by minerals like silica, calcite, or iron oxide.

Uses & applications

Used primarily in the construction industry as a source of aggregate for concrete, as fill material for roads, and occasionally as an ornamental building stone if the patterns are attractive.

Geological facts

Conglomerate is often called 'puddingstone' in certain regions because the rounded pebbles look like raisins in a pudding. It is an indicator of ancient riverbeds or high-energy shoreline environments.

Field identification & locations

Identify in the field by looking for rounded pebbles (clasts) that are larger than 2mm firmly embedded in a finer sandy or silty cement. It is commonly found in sedimentary basins and near mountain fronts.