
sedimentary
Conglomerate
Conglomerate / Lithic Wacke
AI-generated identification · may be incorrectHardness: variable (depends on clasts, often 6-7); Color: grey, brown, tan; Luster: earthy to dull; Crystal structure: clastic (non-crystalline); Specific Gravity: 2.1-2.9
- Hardness
- variable (depends on clasts, often 6-7)
- Color
- grey, brown, tan
- Luster
- earthy to dull
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Physical properties
Hardness: variable (depends on clasts, often 6-7); Color: grey, brown, tan; Luster: earthy to dull; Crystal structure: clastic (non-crystalline); Specific Gravity: 2.1-2.9
Formation & geological history
Formed by the lithification of rounded gravel and pebbles, typically in high-energy environments like riverbeds, beaches, or alluvial fans. Geological age varies widely from Precambrian to Cenozoic.
Uses & applications
Used primarily in the construction industry as coarse aggregate for concrete and road building. Occasionally used as ornamental stone if it contains colorful pebbles.
Geological facts
Conglomerate is often called puddingstone because the rounded pebbles look like raisins in a pudding. It is one of the few rocks that indicates the speed and direction of ancient water currents.
Field identification & locations
Identify in the field by looking for rounded, water-worn pebbles larger than 2mm cemented in a finer-grained matrix. Found globally in ancient river systems and shorelines.
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