Sedimentary rocks are formed by the accumulation and compaction or cementation of sediments. There are three main types - clastic sedimentary rocks which are composed of rock fragments transported by water, wind or ice; chemical sedimentary rocks which form from minerals precipitating from water; and organic sedimentary rocks which are formed from the remains of organisms. Sedimentary rocks can be further classified based on sediment size and include conglomerates, sandstones, shales, evaporites, and coal. They often exhibit layering, ripples, mud cracks, fossils, and concretions.