sedimentary
Conglomerate
Conglomerate (Detrital sedimentary rock)
Hardness: Variable (clasts often approx. 7 Mohs if quartz, matrix 3-5 Mohs); Color: Brown, tan, reddish (iron staining); Luster: Dull/Earthy matrix with waxy/vitreous clasts; Crystal structure: Non-crystalline/Clastic texture; Cleavage: None (breaks around clasts); Specific gravity: 2.6-2.8
- Hardness
- Variable (clasts often approx
- Color
- Brown, tan, reddish (iron staining)
- Luster
- Dull/Earthy matrix with waxy/vitreous clasts
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Physical properties
Hardness: Variable (clasts often approx. 7 Mohs if quartz, matrix 3-5 Mohs); Color: Brown, tan, reddish (iron staining); Luster: Dull/Earthy matrix with waxy/vitreous clasts; Crystal structure: Non-crystalline/Clastic texture; Cleavage: None (breaks around clasts); Specific gravity: 2.6-2.8
Formation & geological history
Formed in high-energy environments like riverbeds, alluvial fans, or beaches where water turbulence is strong enough to transport large rounded pebbles. Over time, these pebbles are buried and cemented by minerals like silica, calcite, or iron oxide. These can range in age from recently lithified to billions of years old.
Uses & applications
Used primarily in the construction industry as coarse aggregate for concrete or as fill material. Historically used as a building stone. Occasionally used decoratively as 'puddingstone' if the clasts are colorful.
Geological facts
Conglomerate is often called 'nature's concrete.' On Mars, NASA's Curiosity rover discovered conglomerate outcrops, providing crucial evidence that liquid water once flowed on the Martian surface in ancient stream-beds.
Field identification & locations
Identify in the field by looking for rounded clasts (pebbles) larger than 2mm diameter held together by a finer-grained matrix. It is found globally in ancient mountain belts and river basins. For collectors, search for 'puddingstone' varieties which contain jasper or colorful quartz clasts.
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