Breccia!

Breccia is a clastic sedimentary rock characterized by its composition of angular fragments or clasts that are cemented together. Here are some key details about breccia:

Formation: Breccia forms in environments where there is little to no transportation of the rock fragments after they are broken off from their source. This can occur in several settings:
Talus Slopes: At the base of cliffs where rockfalls occur, and the fragments accumulate with minimal movement.
Fault Zones: Where tectonic forces break rocks, and the fragments are cemented in place.
Volcanic Eruptions: Around volcanic vents where explosive eruptions eject angular volcanic material.
Submarine Landslides: In underwater environments where landslides deposit broken rock.
Composition:
Clasts: These are the angular fragments, which can be composed of various rock types like limestone, quartzite, or volcanic rocks.
Matrix: The finer material, often sand, silt, or clay, that fills the spaces between the clasts.
Cement: Minerals like calcite, sili