Sedimentary
Compaction and cementation of sediments are the processes of lithification which form clastic sedimentary rock.
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.
It is Limestone Gypsum Coal Dolomite Halite Sandstone Conglomerate Shale
Classic sedimentary rocks are made up a minerals, grains, and rock fragments from older rocks. Some examples of this kind of rock are sandstone, breccia, and shale.
Lithified detritus forms sedimentary rocks known as clastic rocks. These rocks are composed of fragments of pre-existing rocks or minerals, which have been physically weathered and transported before being deposited and compacted into a solid rock. Examples include sandstone, shale, and conglomerate.
Sedimentary rock is produced by the process of deposition and cementation. Examples of sedimentary rocks include sandstone, shale, and limestone.
There is Sandstone, Chalk, Coal, Limestone, and Shale.
Conglomerate
A mix of sandstone and other sediment rocks
Conglomerate is a rock that has pieces of other rocks glued together to form one larger chunk. Therefore, they have a coarse-grained texture
The sedimentary rock formed by burying, compacting, and cementing sediment is called "clastic sedimentary rock." Examples include sandstone, shale, and conglomerate, which are composed of fragments of pre-existing rocks or minerals that have been lithified through the process of compaction and cementation.
Conglomerate is a sedimentary rock formed around other rocks. These other rocks can be any type that is native to the area, or that has been carried from other locations. They are a mixture of different rock types.