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Breccia (Sedimentary) identification and geology

Coarse-grained sedimentary rock composed of angular fragments 2 mm cemented together. Angular clasts indicate minimal transport. Texture: Clastic, angular fragments. Rock type: Sedimentary Clastic. Grain size: Coarse 2 mm, angular. Minerals present: Variable rock fragments, Calcite cement, Silica cement. Formation: Forms from rockfalls, debris flows, fault zones, and collapse of cave roofs. Angular fragments indicate short transport. Common geological settings: Found in fault zones, talus slopes, cave systems, and volcanic regions worldwide. Common look-alikes and related entries: Conglomerate, Agglomerate, Fault Gouge.

Sources, scope & corrections

These authoritative resources support category-level nomenclature, terminology, identification methods, and safety. When a specimen-specific safety warning appears, the public-health source listed here directly supports that precaution. They are not line-by-line citations for every other property on this entry, and natural specimens vary.

Editorial owner
GeoMiner
Last updated
2026-02-10T20:33:30.208882+00:00
Review status
Published; not independently peer-reviewed
  • Rocks — U.S. National Park Service. Authoritative overview of rock groups, the rock cycle, and geologic processes.
  • Can you identify my rock or mineral? — U.S. Geological Survey. Identification limitations and routes to in-person professional verification.

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Common questions

What is Breccia Sedimentary?
Coarse-grained sedimentary rock composed of angular fragments 2 mm cemented together. Angular clasts indicate minimal transport.
How can you identify Breccia Sedimentary?
Compare several properties rather than relying on colour alone. This entry records rock type: Sedimentary Clastic; texture: Clastic, angular fragments; grain size: Coarse 2 mm, angular; common minerals: Variable rock fragments, Calcite cement, Silica cement. Confirm an important identification with additional field tests or qualified laboratory work.
How does Breccia Sedimentary form?
Forms from rockfalls, debris flows, fault zones, and collapse of cave roofs. Angular fragments indicate short transport.
Where is Breccia Sedimentary commonly found?
Found in fault zones, talus slopes, cave systems, and volcanic regions worldwide.
What is Breccia Sedimentary commonly confused with?
Breccia Sedimentary may be confused with Conglomerate, Agglomerate, Fault Gouge. Compare multiple diagnostic properties because colour and surface appearance can overlap.

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