Convection currents in the Earth's mantle are driven by the heat from the core, causing the semi-fluid asthenosphere to flow. These currents play a crucial role in tectonic plate movement, as the asthenosphere's plasticity allows it to move and interact with the overlying lithosphere. As hot material rises and cooler material sinks, it creates a continuous cycle that influences geological processes, including earthquakes and volcanic activity. Thus, convection currents are essential for understanding the dynamics of the asthenosphere and plate tectonics.
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