
sedimentary
Conglomerate
Clastic Sedimentary Rock (Conglomerate)
Hardness: variable (3-7 Mohs); Color: grey to brown; Luster: dull/earthy; Crystal structure: clastic (rounded fragments in a fine-grained matrix); Specific Gravity: 2.1-2.6
- Hardness
- variable (3-7 Mohs)
- Color
- grey to brown
- Luster
- dull/earthy
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Physical properties
Hardness: variable (3-7 Mohs); Color: grey to brown; Luster: dull/earthy; Crystal structure: clastic (rounded fragments in a fine-grained matrix); Specific Gravity: 2.1-2.6
Formation & geological history
Formed in high-energy environments like riverbeds or alluvial fans where water currents are strong enough to transport large rounded pebbles, which are then cemented together over geological time.
Uses & applications
Used primarily in the construction industry as coarse aggregate for concrete, as a decorative stone in architecture, and occasionally as a base material for roads.
Geological facts
Conglomerates are often referred to as 'puddingstone' because the rounded clasts resemble raisins in a pudding. They are key indicators of ancient water flow and shoreline positions.
Field identification & locations
Identify by looking for rounded pebbles or cobbles larger than 2mm embedded in a finer matrix of sand or silt. Found globally in ancient riverbeds and mountain fronts.
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