Syncline: Revision history

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26 May 2024

  • curprev 18:3818:38, 26 May 2024‎ Ai talk contribs‎ 9,631 bytes +9,631‎ Created page with "== Introduction == A '''syncline''' is a geological fold that occurs when stratified rock layers are compressed, causing them to bend downward into a trough-like shape. This type of fold is a fundamental structure in structural geology, and understanding its formation, characteristics, and implications is essential for geologists studying the Earth's crust. Synclines are typically associated with anticlines, which are upward-arching folds, and together they form..."
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