The evidence supporting the theory of continental drift includes continental fit, Glossopteris Flora fossils, and seafloor spreading.
Continental Fit: The coasts of western Africa and eastern South America looked like the edges of interlocking pieces of a jigsaw puzzle, supporting the idea that they were once connected.
Glossopteris Flora: Evidence from Glossopteris fossils found across South America, Africa, Antarctica, India, and Australia suggesting these landmasses were once connected as part of a supercontinent.
Seafloor Spreading: The process of new crust forming between moving plates causing continents to drift apart, supported by discoveries like the Tharp-Heezen map revealing seafloor spreading.
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