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Tillite is a lithified till (poorly sorted glacial debris) which may be called a matrix-supported conglomerate if there are enough granules, pebbles, cobbles, and boulders present. At least 30% of the rock should be composed of clasts larger than 2 mm in diameter in order to call that rock a true conglomerate.Conglomerate from the Ordovician near Bergen in Norway. The clasts are made of quartzite and are slightly flattened due to metamorphism.onglomerate is composed of clasts larger than 2 mm which is the upper limit of sand grains size. Conglomerates are differentiated from sedimentary breccias which are composed of angular clasts.
Breccia is a clastic sedimentary rock composed of angular fragments of rocks and rock particles that have been lithified (cemented together). Breccia also has large fragments of rock.Conglomerate is a clastic sedimentary rock composed of rounded fragments of rocks and rock particles that have been lithified.Breccia is usually formed closer geographically to the point of origin of the rock fragments than are the rock fragments in conglomerate.reccia is a clastic sedimentary rock composed of angular fragments of rocks and rock particles that have been lithified (cemented together). Breccia also has large fragments of rock.