The hot cocoa/wax model effectively illustrates the relationship between Earth's mantle and tectonic plates by using the properties of density and convection currents.
In this model, the cold water represents the mantle, which is generally cooler and denser than the hot cocoa. The hot cocoa (or wax) simulates the convection currents within the mantle, as it is heated and rises due to being less dense when warmed. As the hot cocoa rises, it represents the movement of material in the mantle that drives the motion of tectonic plates on the surface.
When the hot cocoa cools, it becomes denser and sinks back down, illustrating how the mantle material cycles through convection currents. This cycle demonstrates how tectonic plates float on the mantle and are moved by the dynamic processes occurring beneath them due to these convection currents.
Therefore, the correct understanding of the model is:
The cold water represented the mantle, while the floating cocoa/wax showed how tectonic plates move due to density differences and convection currents.