Distinctive
features:
Similar to conglomerate, but rock fragments
are angular and set in fine-grained matrix.
Distinguish from agglomerate (volcanic
equivalent) by its sedimentary origin.
Colour:
Variable,
depending on the type of rock fragments.
Texture and
granularity:
Angular fragments
of rock set in fine grained matrix.
Composition:
Fragmented rocks
of any kind can form breccia. The matrix is
normally fine sand or silt, cemented by
secondary silica or calcite.
Field
associations:
Derived from
scress and fault zones. Often found near conglomerate, arkose and sandstone.
Varieties:
Named according to rock type of which it is
composed.