Rock Identifier
Conglomerate (Clastic sedimentary rock (Polymict conglomerate with quartz/calcite matrix)) — sedimentary
sedimentary

Conglomerate

Clastic sedimentary rock (Polymict conglomerate with quartz/calcite matrix)

Hardness varies by components (typically 6-7 for quartz pebbles), variable colors featuring brownish-red rounded clasts in a lighter matrix, dull to earthy luster, fragmental structure with no true cleavage, specific gravity around 2.5-2.7

Identified More sedimentary
Explore Conglomerate in the encyclopedia →

Identify your own rocks.

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

Physical properties

Hardness varies by components (typically 6-7 for quartz pebbles), variable colors featuring brownish-red rounded clasts in a lighter matrix, dull to earthy luster, fragmental structure with no true cleavage, specific gravity around 2.5-2.7

Formation & geological history

Formed by the consolidation and cementation of gravel-sized and rounded clasts, often deposited in high-energy environments like fast-flowing rivers, alluvial fans, or beach zones over millions of years

Uses & applications

Used primarily in the construction industry as crushed stone for road aggregate and building foundations, and occasionally as decorative stone or educational display pieces

Geological facts

Conglomerates are often referred to as 'nature's concrete' because they consist of natural gravels and boulders cemented together by finer minerals like silica, calcite, or iron oxide

Field identification & locations

Easily identified in the field by its distinct 'plum-pudding' texture of rounded pebbles embedded in a finer matrix; commonly found in sedimentary basins and riverbeds worldwide