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This document discusses the principles of stratigraphy used by geologists to interpret the geological history of a region. It describes several key stratigraphic laws and concepts, including: - Original horizontality, which states that sedimentary rock layers are deposited horizontally. Tilted layers have been deformed after deposition. - Lateral continuity, which describes how sedimentary layers extend horizontally across a region as continuous sheets unless depositional conditions change. - Superposi

Author

Grida Viantiska

Language

EN