Continental drift is the hypothetical situation that assumes that the Earth's continents have moved over the geological time in relation to each other, this shows the drifting of the ocean bed across the globe.
The fossils are the most important evidence for knowing the idea of continental drifts because it was strongly supported by the Theory of Continental Drifts.
For knowing the continental drift the current climate and prehistoric climate of the fossil is necessary to understand as it helps to know the particles included in the fossil that affects the happening of the drifts. The current climate shows the effect of the fossil over the drift and the prehistoric climate shows the changes in the current climate due to previous prehistoric climate changes.
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