sedimentary
Breccia
Breccia - Clastic sedimentary rock
Hardness varies based on matrix (often 6-7 if siliceous); Color: Multi-colored with dark angular fragments in a lighter tan or white matrix; Luster: Dull to earthy; Texture: Clastic with angular fragments larger than 2mm.
- Luster
- Dull to earthy
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Physical properties
Hardness varies based on matrix (often 6-7 if siliceous); Color: Multi-colored with dark angular fragments in a lighter tan or white matrix; Luster: Dull to earthy; Texture: Clastic with angular fragments larger than 2mm.
Formation & geological history
Formed by the accumulation of angular fragments of rock or mineral debris cemented together. This process typically occurs in high-energy environments like base of cliffs (talus), fault zones (fault breccia), or volcanic events.
Uses & applications
Used primarily as decorative architectural stone, road base material, and occasionally in jewelry as cabochons if the matrix and inclusions are aesthetically pleasing.
Geological facts
The key difference between breccia and conglomerate is the shape of the fragments; breccia has angular pieces, indicating they haven't traveled far from their source, whereas conglomerate has rounded pieces.
Field identification & locations
Identified by the large, sharp-angled rocky fragments cemented in a finer-grained matrix. Look for it at the base of outcrops or along fault lines. Collectors value specimens with high color contrast.
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