sedimentary
Conglomerate
Conglomerate (SiO2 matrix with various silicate clasts)
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.
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Physical properties
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.
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.
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