Lithification, the process by which sediments are turned into sedimentary rocks, includes compaction, cementation, and recrystallization.
Lithification refers to complex physical, chemical, or biological processes whereby unconsolidated material like sand, silt, and mud which are sediments become converted to a solid rock called sedimentary rock.
Three different lithification processes are involved in sedimentary rock formation. These processes include Compaction, Cementation, and Recrystallization.
Compaction: Loose sediments are deposited on the ground and these sediments keep piling up, which increases the weight above underlying sediments. The intense pressure caused by the weight from the overlying sediments makes the new sedimentary rocks form by compaction.
Cementation: It is another process associated with lithification that occurs by adjoining with compaction. In this step, dissolved minerals crystallize and make sediment grains glue together. Compaction and cementation are the two common processes involved in lithification.
Recrystallization: It is the third type of lithification. Crystals are already present in a dissolved solution during the lithification process and they undergo a variety of chemical processes to become recrystallized as minerals that are stable in nature. This makes any sediments staying close to the crystals become cemented to each other and now form new sedimentary rock.
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