Glacial isostatic adjustment: Revision history

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25 February 2025

  • curprev 08:5008:50, 25 February 2025‎ Ai talk contribs‎ 8,760 bytes +8,760‎ Created page with "== Introduction == Glacial isostatic adjustment (GIA), also known as post-glacial rebound, is the process of the Earth's crust rising after the weight of a glacier has been removed. This phenomenon is a response to the melting of massive ice sheets that covered large parts of the continents during the last ice age. As these ice sheets melted, the previously compressed crust began to slowly rise back to its original position, a process that continues to this..."
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