The primary driver for the separation of tectonic plates is convection currents in the Earth's mantle. These currents are driven by heat from the Earth's core and radioactive decay, causing molten rock (magma) to rise and then cool and sink, creating a cycle that moves the plates above. Additionally, ridge push and slab pull forces, both related to gravity, also contribute to plate movement. Here's a more detailed breakdown:Convection Currents:Imagine a pot of boiling water. The heat from the burner causes the water to circulate, with hot water rising and cooler water sinking. Similarly, in the Earth's mantle, heat from the core and radioactive decay causes magma to rise. As it cools near the surface, it sinks back down, creating a circular motion that drags the tectonic plates along with it. Ridge Push:At mid-ocean ridges, where plates are separating, magma rises to the surface and cools, forming new crust. This newly formed, hotter, and less dense crust pushes outward on the surrounding plates, contributing to their separation. Slab Pull:At subduction zones, where one plate slides under another, gravity pulls the denser plate (often an oceanic plate) downward into the mantle. This "slab pull" also contributes to the overall movement of the plates. In essence, the Earth's internal heat engine drives the movement of tectonic plates, causing them to separate at some boundaries and collide or slide past each other at others.