They cause plate movement. The plate movement then causes an earthquake.
No, convection currents in the mantle are the primary driving force behind the movement of tectonic plates. These currents are generated by heat from the Earth's core, causing movement in the mantle that in turn drags and moves the overlying tectonic plates.
the movement of convection currents in the mantle is the cause of plate motion.
the movement of convection currents in the mantle is the cause of plate motion.
Convection currents in the mantle transfer heat, causing the movement of tectonic plates above. This movement results in phenomena such as earthquakes, volcanoes, and mountain building as plates collide, separate, or slide past each other. The crust itself is not responsible for the movement, but rather is driven by the convection currents in the underlying mantle.
the movement of convection currents in the mantle is the cause of plate motion.
the movement of convection currents in the mantle is the cause of plate motion.
the movement of convection currents in the mantle is the cause of plate motion.
the movement of convection currents in the mantle is the cause of plate motion.
The difference in temperature and density is the cause of convection currents in the earths mantle. Convection currents are the flow that transfers heat within a fluid.
The difference in temperature and density is the cause of convection currents in the earths mantle. Convection currents are the flow that transfers heat within a fluid.
Most convection currents that cause seafloor spreading are thought to be located in the asthenosphere, which is a semi-fluid layer of the Earth's upper mantle beneath the lithosphere. The movement of these convection currents is believed to drive the motion of tectonic plates.
Scientists believe that convection currents flow through the Earth's mantle, which is the layer of hot, flowing rock beneath the Earth's crust. These currents are driven by heat from the Earth's core and cause the movement of tectonic plates at the surface.