
sedimentary
Conglomerate
Clastic sedimentary rock (Conglomerate)
Hardness: 6.5-7 (typically mirrors the hardness of the quartz matrix), Color: Reddish-brown with embedded dark grey and tan clasts, Luster: Dull/Earthy, Crystal Structure: Clastic (non-crystalline), Cleavage: None (fractures around clasts), Specific Gravity: 2.6-2.8
- Hardness
- 6
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Physical properties
Hardness: 6.5-7 (typically mirrors the hardness of the quartz matrix), Color: Reddish-brown with embedded dark grey and tan clasts, Luster: Dull/Earthy, Crystal Structure: Clastic (non-crystalline), Cleavage: None (fractures around clasts), Specific Gravity: 2.6-2.8
Formation & geological history
Formed in high-energy environments like riverbeds, alluvial fans, or beaches where water currents are strong enough to transport large, rounded pebbles. Over time, these pebbles are buried and cemented by minerals like calcite or silica. This specimen likely dates from the Phanerozoic eon.
Uses & applications
Commonially used as a coarse aggregate in the construction industry for concrete and road beds. Higher-quality, colorful specimens are sometimes cut as 'puddingstone' for ornamental use or lapidary work.
Geological facts
Conglomerate is often called 'nature's concrete.' On Mars, NASA's Curiosity rover discovered conglomerate outcrops, providing key evidence that vigorous ancient streams once flowed across the Martian surface.
Field identification & locations
Identify by looking for rounded pebbles (clasts) larger than 2mm firmly embedded in a finer-grained matrix. Unlike Breccia, which has angular fragments, Conglomerate fragments are rounded by water erosion. Common in sedimentary basins worldwide.
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