January 8, 2025
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0:53Now PlayingThe 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.
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#IsostaticRebound #Deglaciation #PlateTectonics #EarthAdjustments
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