The discussion centers on the hypothetical scenario of Earth's core being larger, occupying 70% of its radius, and the implications for plate tectonics. It highlights that plate tectonics is primarily driven by mantle convection, which is influenced by heat generated in the Earth's core. A larger core could potentially produce more heat, leading to stronger mantle convection and possibly more active plate tectonics. However, the conversation acknowledges the speculative nature of this hypothesis, emphasizing that such questions may fall outside the strict scientific method due to their hypothetical nature. The role of various heat sources, including radiogenic heat and friction between the core and mantle, is also considered, though the exact effects of a larger core on these heat sources remain uncertain.