The correct response that effectively describes how superheated magma is transferred up to the Earth's crust and creates convection currents is:
D. The deep, hot magma becomes less dense than the cooler, upper mantle rocks and it rises. At the same time, the magma close to the surface cools and sinks to replace the rising magma. This movement creates convection currents.
This explanation accurately captures the process of convection, which is the primary mechanism by which heat and materials move in fluids (including molten rock) due to differences in density. The hot magma, being less dense, rises toward the crust, while the cooler, denser magma sinks, resulting in the cyclical movement that forms convection currents in the mantle.