Geology and Minerals

Cataclasite

Cataclasite is a cohesive granular fault rock. Comminution, also known as cataclasis, is an important process in forming cataclasites. They fall into the category of cataclastic rocks which are formed through faulting or fracturing in the upper crust. Cataclasites are distinguished from fault gouge, which is incohesive, and fault breccia, which contains coarser fragments.

Also on this shelf

See also

• ▸Geology and geological history of California
• ▸Karl Jenkins
• ▸Chuska Mountains

Uncatalogued shelf

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