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Stratification is the process of forming layers of sedimentary rocks through erosion, weathering, and deposition of particles over time. Key laws of stratigraphy, such as the Law of Superposition and the Law of Faunal Succession, help in understanding the age and correlation of rock layers. The key stages of stratification include weathering, erosion, deposition, compaction, and cementation, leading to the formation of distinct strata.

Author

Franzmae Lianne

Language

EN