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Upwelling Mantle
Refers to the process where hotter, less dense mantle material ascends towards the Earth's surface, typically at mid-ocean ridges or hotspots.
Mantle Convection
Movement of mantle material in response to variations in density, especially those caused by differences in temperature.
Asthenosphere
A semi-fluid layer beneath the Earth's lithosphere on which the tectonic plates move, located in the upper mantle between approximately 100 and 250 kilometers deep.
Density
A measure of mass per unit volume of a substance, influencing how materials interact, such as floating or sinking in water.
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