sedimentary

Conglomerate

Conglomerate (SiO2 matrix with various silicate clasts)

AI-generated identification · may be incorrect

Hardness varies (generally 6.5-7 for quartz-rich specimens), color is a mix of tan, brown, and dark gray clasts, luster is dull to waxy, clastic texture with rounded gravel-sized fragments, no specific crystal structure for the whole rock.

Identified April 26, 2026More sedimentary →

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Physical properties

Formation & geological history

Formed in high-energy environments like riverbeds or alluvial fans where water rounds large rock fragments. These fragments are then buried and cemented together by minerals like silica or calcite over millions of years.

Uses & applications

Used primarily as aggregate in construction, road base, and occasionally as a decorative stone in landscaping or architectural cladding.

Geological facts

Conglomerate is often called "puddingstone" because the rounded rocks look like raisins or plums in a pudding. It is the sedimentary equivalent of a 'breccia' which contains angular rather than rounded fragments.

Field identification & locations

Identify in the field by looking for large, rounded pebbles or cobbles (clasts) that are permanently stuck together in a finer-grained matrix. Common in ancient river basins and coastal areas.