Breccia is a clastic sedimentary rock composed of broken angular fragments of minerals or rock cemented together by a fine-grained matrix. Unlike conglomerate, the particles in breccia are sharp and angular, indicating they have not traveled far from their source before lithification.
Is this breccia?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch breccia with a known reference. Breccia sits at Mohs 3-7 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Breccia leaves a variable streak.
- 3Read the lusterHold the specimen under a strong light. Breccia typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: gray, brown, red, white, variegated.
- 5Look at form & habitTypical habit: massive.
Often confused with
Breccia vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside breccia
Minerals reported to co-occur with breccia. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 3-7
- Density
- 2.0-2.8 g/cm³
- Streak
- Variable
- Luster
- Dull
- Transparency
- Opaque
- Crystal habit
- Massive
- Cleavage
- None
- Rarity
- Common
- Uses
- Decorative, Architectural, Collector
- Host rock
- Sedimentary Basins, Fault Zones, Volcanic Pipes
- Typical price
- $5-50 for small polished samples, higher for large decorative slabs.
Where rockhounds find breccia
Classic worldwide localities
- worldwide
- Italy
- Greece
- USA
Field-hunting tip
Look in sedimentary basins, fault zones, volcanic pipes country — that is the host setting where breccia typically forms. If you start seeing calcite, quartz, limonite in float, you are in the right ground. Field specimens usually show a massive habit, so train your eye for that shape before scanning the outcrop.




