Option A
Continental Drift Theory
This theory highlighted how big continents were broke down into smaller one It was discovered by Alfred Wegener in 1912.
Some common evidences are movement of fossils remains
for example -
Fossil plant Glossolalia and reptile Lystrosaurus found today in South America, Africa, India, Antarctica, and Australia were part of Giant Gondwana Island which broke of from Pangaea about 200 million years ago. He also emphasizes that convection currents produced due to rising of hot rock over the mid-ocean ridges, and then sinks down as it cools and becomes denser. Due to this arrangement magnetism effect can be seen in earth crust