Weathering and erosion from an existing rock, transportation and deposition, compaction and cementation.
lithification
Fragmentation clastic sedimentary rock is formed by the lithification of inorganic and/or organic sediments.
Crystalline rock is composed of interlocking crystalline grains, as in granite. Clastic rock is composed of rock or mineral grains which have become cemented together by the processes of lithification. Examples of clastic rock are sandstone and conglomerate.
Fragmentation clastic sedimentary rock is formed by the lithification of inorganic and/or organic sediments.
Fragmentation clastic sedimentary rock is formed by the lithification of inorganic and/or organic sediments.
They are classified as clastic or non-clastic. Clastic sedimentary rocks are formed from rock particles of various sizes. Non-clastic rocks are formed from precipitation of minerals out of solution or by the lithification of organic matter.
When rock sediment is lithified, a sedimentary rock is formed. The two processes involved in lithification are compaction and cementation.
If existing bits of rock become attached through the process of lithification, a clastic sedimentary rock is formed.
Clastic sediments are sediments that have particles or pieces of rock (clasts) in them. The clasts can be of igneous, metamorphic or sedimentary rock. Non-clastic sediments are made up of dissolved minerals or organic matter.
The formation of a clastic sediment and sedimentary rocks involves five processes: 1. weathering 2. erosion 3. transportation 4. deposition 5. lithification
Compaction and cementation of sediments are the processes of lithification which form clastic sedimentary rock.
The chemical sedimentary rock will not be composed of cemented rock particles.