Sandstone
sandstoneshalesiltstonemudstonelimestonecoaletc.
Chalk and coal are examples of a kind of sedimentary rock called biochemical sedimentary rock. Biochemical sedimentary rocks form from the accumulation and lithification of organic remains, such as shells and plant material.
sedimentary rock and igenous rock.
Soil is a non-example of a sedimentary rock.
Rock salt and rock gypsum are common examples of a group of chemical sedimentary rocks called evaporities. When a sedimentary rock consists of angular, grave sized particles is breccia.
Sandstone, limestone, shale.
Sedimentary rock forms from the layering of eroded rock material, which accumulates and undergoes compaction and cementation over time. Examples of sedimentary rocks include sandstone, shale, and limestone.
Shale, sandstone, and conglomerate are examples of clastic sedimentary rock.
From biological processes: organic sedimentary rock.From precipitation or evaporation: chemical sedimentary rock.
Some examples of chemical sedimentary rocks include limestone, dolostone, and rock salt. These rocks form when minerals precipitate out of a solution, such as when water evaporates or through processes like precipitation.
A sedimentary rock is formed when rock fragments are compacted and cemented together by pressure and minerals. Examples of sedimentary rocks include sandstone, shale, and conglomerate.
They are called chemical sedimentary rocks. Rock salt and rock gypsum are two examples.