The particles in breccia are primarily silt sized.

Name: The particles in breccia are primarily silt sized.
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Breccia is a type of sedimentary rock that is composed of larger, angular fragments (greater than 2 mm in size) that are cemented together. The particles in breccia are not primarily silt sized, but rather, they are larger and more irregular in shape. Silt-sized particles would typically be found in rocks such as siltstone or shale.

The Particles in Breccia Are Primarily Silt Sized