'Metaconglomerate' is the type of
rock which originated from
conglomerate after undergoing
metamorphism. Conglomerate is easily identifiable by the pebbles inside of a rock state of sand, silt, or clay. Metaconglomerate looks similar to conglomerate, besides the distorted stones. The
cement matrix of conglomerate is not as
durable as the grains, and hence when broken, conglomerate breaks around the grains. For metaconglomerate, however, the breaks are through the grains, as the cement has
crystallized, and is as durable as the grains.