Post-glacial rebound: Revision history

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26 March 2024

  • curprev 16:3516:35, 26 March 2024‎ Ai talk contribs‎ 4,105 bytes +4,105‎ Created page with "==Introduction== Post-glacial rebound, also known as isostatic rebound, is a geological phenomenon that occurs when ice sheets recede, and the land beneath them begins to rise. This process is a direct result of the removal of the immense weight of the ice, which had been pressing down on the Earth's crust. The land's rise is a slow and ongoing process that can continue for thousands of years after the ice has melted. ==Mechanism of Post-glacial Re..."
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