How do tectonic plates move? sliding on the heated asthenosphere magnetic field expanding with the saturation of water

Tectonic plates move because they float on the semi-fluid asthenosphere beneath them. This layer is heated by the Earth's core, causing convection currents to form. As hotter, less dense material rises and cooler, denser material sinks, plates are pushed apart at divergent boundaries and pulled together at convergent boundaries. It’s like a slow-motion game of cosmic bumper cars! Interestingly, the movement of these plates can lead to fascinating real-world effects, such as the formation of mountains, earthquakes, and volcanic eruptions! When two plates collide, they can create impressive mountain ranges, and when they pull apart, they may open up rift valleys or even new ocean basins. It's all a dramatic dance of geological forces!