sedimentary
Conglomerate
Clastic sedimentary rock (Conglomerate)
Hardness: 6-7 (depending on clast types like quartz); Color: Gray, green-gray matrix with tan/brown clasts; Luster: Dull/Earthy; Structure: Clastic, containing rounded pebbles (clasts) cemented in a fine-grained matrix.
- Hardness
- 6-7 (depending on clast types like quartz)
- Color
- Gray, green-gray matrix with tan/brown clasts
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 (depending on clast types like quartz); Color: Gray, green-gray matrix with tan/brown clasts; Luster: Dull/Earthy; Structure: Clastic, containing rounded pebbles (clasts) cemented in a fine-grained matrix.
Formation & geological history
Formed in high-energy environments like riverbeds or alluvial fans where water current is strong enough to transport large pebbles. Over time, these pebbles are deposited and cemented by minerals like silica or calcite.
Uses & applications
Used primarily as heavy-duty construction aggregate, fill material in road building, or as ornamental 'river stones' in landscaping.
Geological facts
Conglomerate is often called a 'rock pudding' due to its appearance. Mars Curiosity Rover found conglomerate rocks on Mars, proving that ancient rivers once flowed there.
Field identification & locations
Identify in the field by looking for rounded, smooth pebbles larger than 2mm embedded in a finer matrix. Often found in old river valleys or coastal areas.
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