Breccia is clastic.
Breccia is clastic.
Breccia is a clastic sedimentary rock.
Breccia is typically a nonfoliated rock, meaning that it lacks the aligned mineral grains or bands characteristic of foliated rocks. Breccia forms from the cementation of broken rock fragments, giving it a distinct angular appearance.
Breccia
Breccias are a relatively common clastic sedimentary rock.
Breccia.
Breccia is a sedimentary rock that is composed of large angular fragments of various rocks cemented together by a fine-grained matrix. These fragments are typically a mix of different minerals and rock types, giving breccia a diverse appearance.
Breccia can have varying levels of hardness depending on the composition of the rock fragments and the cementing material holding them together. Generally, breccia is considered to be moderately hard to hard.
Breccia usually has a dull to earthy luster due to its composition of angular rock fragments and matrix. The luster of breccia can vary depending on the types of rocks it contains and the amount of matrix present.
Breccia is a coarse-grained sedimentary rock that is composed of large, angular fragments.
Breccia.
Breccia and conglomerate are detrial.