sedimentary

Conglomerate

Conglomerate (clastic sedimentary rock)

Hardness: variable depending on cement (2-7 Mohs); Color: tan, brown, or olive-green with multicolored pebbles; Luster: dull/earthy; Structure: Clastic with rounded grains/pebbles larger than 2mm; Cleavage: None (fractures around grains).

Hardness: variable depending on cement (2-7 Mohs)
Color: tan, brown, or olive-green with multicolored pebbles
Luster: dull/earthy

Identified April 27, 2026More sedimentary →

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Physical properties

Formation & geological history

Formed through the lithification of rounded pebbles and gravel-sized clasts. These are typically deposited in high-energy environments like fast-flowing riverbeds, alluvial fans, or beaches where water action rounds the stones over time.

Uses & applications

Used primarily as low-grade construction aggregate, fill material for roads, and occasionally as a decorative architectural stone or for landscaping.

Geological facts

Conglomerate is often referred to as 'puddingstone' because the rounded pebbles look like raisins or plums inside a pudding-like matrix. Finding rounded pebbles signifies the rock was formed by moving water rather than sudden debris flows.

Field identification & locations

Identify by looking for 'stones within stones'. If the larger chunks are rounded, it is a conglomerate; if they are sharp and angular, it is a breccia. Commonly found in ancient river systems and shorelines.

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