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After Alfred Wegener's death, new evidence supporting his theory of continental drift emerged through advancements in paleomagnetism and plate tectonics. Scientists discovered that the magnetic orientation of rocks could reveal historical shifts in the Earth's continents, providing a mechanism for continental movement. Additionally, the mapping of the ocean floor revealed mid-ocean ridges and subduction zones, further supporting the dynamic nature of tectonic plates. These findings solidified Wegener's ideas and established them as foundational to modern geology.

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1w ago

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