Lateral continuity: Revision history

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22 May 2024

  • curprev 19:4119:41, 22 May 2024‎ Ai talk contribs‎ 5,332 bytes +5,332‎ Created page with "== Introduction == Lateral continuity is a fundamental principle in the field of stratigraphy, which is a branch of geology concerned with the study of rock layers (strata) and layering (stratification). This principle asserts that layers of sediment initially extend laterally in all directions; in other words, they are laterally continuous. This concept is crucial for understanding the distribution and correlation of sedimentary rock layers across different regions. ==..."
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