
sedimentary
Conglomerate
Sedimentary Conglomerate
Hardness typically varies from 6 to 7 depending on the constituent pebbles (often quartz). Color is typically brown, tan, or multicolored. Luster is dull to earthy. Composed of rounded to sub-rounded gravel-sized clasts set in a finer-grained matrix of sand, silt, or clay.
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Physical properties
Hardness typically varies from 6 to 7 depending on the constituent pebbles (often quartz). Color is typically brown, tan, or multicolored. Luster is dull to earthy. Composed of rounded to sub-rounded gravel-sized clasts set in a finer-grained matrix of sand, silt, or clay.
Formation & geological history
Formed by the consolidation and cementation of gravel and rounded fragments of rock, transported by high-energy water currents in rivers, streams, or coastal environments, and deposited over millions of years.
Uses & applications
Used primarily in the construction industry as crushed stone for road base, concrete aggregate, and sometimes as an architectural or decorative building stone.
Geological facts
Conglomerates are often referred to colloquially as 'puddingstone' because their appearance resembles a plum pudding containing pieces of fruit embedded in a batter. The degree of rounding of the clasts indicates the distance the material was transported by water.
Field identification & locations
Easily identified by its distinctive 'gravel embedded in concrete' appearance. It is found worldwide in sedimentary basins, river beds, and ancient alluvial fans.
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Sedimentary Sandstone
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Banded Siltstone / Mudstone Pebble
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