The rapid deglaciation at the end of the last ice age triggered isostatic rebound, where Earth’s crust adjusts as glaciers retreat. This process shifts the crust’s distance from the planet’s center of gravity, creating disequilibrium. As an oblate spheroid, Earth’s surface adjusts to restore balance, leading to significant tectonic activity and compensatory changes over time. | The Randall Carlson
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The rapid deglaciation at the end of the last ice age triggered isostatic rebound, where Earth’s crust adjusts as glaciers retreat. This process shifts the crust’s distance from the
The Randall Carlson. The Randall Carlson · Original audio. The rapid deglaciation at the end of the last ice age triggered isostatic rebound, where Earth’s crust adjusts as glaciers retreat. This process shifts the crust’s distance from the planet’s center of gravity, creating disequilibrium. As an oblate spheroid, Earth’s surface ...
141.9K viewsJan 8, 2025
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