Mantle convection is the very slow creep of Earth's solid silicate mantle as convection currents carry heat from the interior to the planet's surface. Types of convection · Creep in the mantle |
Mantle convection is the main way heat from Earth's interior is transported to its surface, and this heat escapes principally through mid-ocean ridges. |
Mantle convection refers to the process in which the Earth's mantle undergoes convective flow, causing gravity anomalies. |
Convection currents are heat-driven cycles that occur in the air, ocean, and mantle. They are caused by a difference in temperature, often due. |
Convection currents within Earth's mantle form as material near the core heats up. As the core heats the bottom layer of mantle material, particles move more ... |
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