
sedimentary
Conglomerate
Conglomeratic Sandstone
Hardness: 6-7 (based on quartz content); Color: Tan, brown, and white clasts; Luster: Dull/Earthy; Structure: Clastic; Cleavage: None; Specific Gravity: 2.6-2.8.
- Hardness
- 6-7 (based on quartz content)
- Color
- Tan, brown, and white clasts
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 (based on quartz content); Color: Tan, brown, and white clasts; Luster: Dull/Earthy; Structure: Clastic; Cleavage: None; Specific Gravity: 2.6-2.8.
Formation & geological history
Formed in high-energy environments like riverbeds or alluvial fans where rounded gravel and pebbles are cemented together by finer grains of sand or silt.
Uses & applications
Used primarily as coarse aggregate for road construction, fill material, and occasionally as decorative building stone.
Geological facts
Conglomerates are often referred to as 'puddingstone' because they resemble fruit pudding. They provide records of ancient river systems and paleo-environments.
Field identification & locations
Identify by the presence of rounded rocky clasts bigger than 2mm embedded in a finer sandy matrix. Commonly found in sedimentary basins and mountain foothills.
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