
sedimentary
Conglomerate
Conglomerate (clastic sedimentary rock)
Hardness: variable (depends on clast type, usually 6-7 for quartz fragments); Color: tan, brown, or grey matrix with multi-colored rounded pebbles; Luster: dull/earthy; Structure: clastic texture with rounded fragments >2mm in diameter.
- Luster
- dull/earthy
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Physical properties
Hardness: variable (depends on clast type, usually 6-7 for quartz fragments); Color: tan, brown, or grey matrix with multi-colored rounded pebbles; Luster: dull/earthy; Structure: clastic texture with rounded fragments >2mm in diameter.
Formation & geological history
Formed through the lithification of rounded gravel and pebbles, typically in high-energy environments like river beds, alluvial fans, or beaches where water movement rounds the stones over time.
Uses & applications
Primarily used as a coarse aggregate in the construction industry for concrete and roads; occasionally used as decorative stone in landscaping or interior design.
Geological facts
Conglomerate is often called 'puddingstone' because the rounded stones embedded in the matrix look like raisins in a pudding. It is an indicator of ancient high-energy water systems.
Field identification & locations
Identify by looking for large, rounded rock fragments cemented together in a finer matrix. Common in sedimentary basins worldwide. It differs from breccia, which contains angular fragments.
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