Marl - Wikipedia Marl is an earthy material rich in carbonate minerals, clays, and silt When hardened into rock, this becomes marlstone It is formed in marine or freshwater environments, often through the activities of algae
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Marl - Geology is the Way Marls are sedimentary rocks with mixed composition, consisting in part of carbonate sediment (carbonate ooze) and in part of fine-grained siliciclastic sediment (clay and silt)
MARL Definition Meaning - Merriam-Webster The meaning of MARL is a loose or crumbling earthy deposit (as of sand, silt, or clay) that contains a substantial amount of calcium carbonate
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