Physical evidence supporting the theory of tectonic plates and continental drift includes the fit of continental Coastlines, particularly the jigsaw-like match between South America and Africa. Additionally, fossil correlations, such as similar species found on widely separated continents, provide evidence of past connectivity. Geological formations, like mountain ranges and rock types that align across continents, further support the idea of once-cohesive landmasses. Lastly, the distribution of earthquakes and volcanic activity along plate boundaries illustrates the movement and interaction of tectonic plates.
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