sedimentary

Sedimentary Breccia

Breccia (Clastic Sedimentary Rock)

AI-generated identification · may be incorrect

Hardness: 6-7 (if quartz-rich); Color: Gray matrix with reddish-brown angular clasts; Luster: Dull/Earthy; Structure: Clastic with angular rock fragments; Specific Gravity: 2.6-2.7

Hardness: 6-7 (if quartz-rich)
Color: Gray matrix with reddish-brown angular clasts
Luster: Dull/Earthy

Identified March 11, 2026More sedimentary →

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Physical properties

Hardness: 6-7 (if quartz-rich); Color: Gray matrix with reddish-brown angular clasts; Luster: Dull/Earthy; Structure: Clastic with angular rock fragments; Specific Gravity: 2.6-2.7

Formation & geological history

Formed through the accumulation of angular fragments of other rocks or minerals that have not been rounded by water. They are typically created in high-energy environments like debris flows, fault zones, or along the base of steep slopes where sedimentation is rapid.

Uses & applications

Primarily used in construction as road base, architectural stone, and occasionally for decorative floor tiles or countertops due to its interesting visual texture.

Geological facts

Unlike conglomerate rocks, which have rounded pebbles, breccia's sharp corners indicate that the fragments have not traveled far from their source before being cemented together.

Field identification & locations

Identify in the field by looking for 'broken' rock pieces larger than 2mm embedded in a finer-grained matrix. Found commonly at the base of talus slopes, in karst areas, or along tectonic fault lines.