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Sediments are classified based on their particle size. There are four main categories of siliciclastic sedimentary particles: major minerals, accessory minerals, rock fragments, and chemical sediments. Sediments are named based on whether they are loose or consolidated into rock. Loose sediments include boulder, cobble, pebble, sand, silt, and clay depending on their size range. The corresponding consolidated rocks are conglomerate/breccia, gravel, sandstone, siltstone, and claystone/mudstone/shale. Carbonate sediments are comprised of minerals like aragonite, calcite, and dolomite. They generally form limestone when lithified, but can also form dolom










