The mantle is hotter than the crust.
No, the core is hotter.
Heat transfer from the mantle creates convection currents that drive the movement of Earth's crustal plates. As hotter mantle material rises, it pushes the crust apart at mid-ocean ridges, while cooler material sinks, pulling the crust down in subduction zones. This movement of the crust is known as plate tectonics.
The mantle is expected to be cooler than the inner core but hotter than the outer core. The inner core is the hottest layer of the Earth, while the outer core is composed of molten iron and nickel. The mantle, located between the crust and core, experiences convection currents due to heat from the core, making it warmer than the outer core but cooler than the inner core.
The mantal
Yes
No, the core is hotter.
Yes it is
Heat transfer from the mantle creates convection currents that drive the movement of Earth's crustal plates. As hotter mantle material rises, it pushes the crust apart at mid-ocean ridges, while cooler material sinks, pulling the crust down in subduction zones. This movement of the crust is known as plate tectonics.
The mantle is definately not hotter that the inner core. i know this because we are doing this at school and if the mantle is hotter we could not live on the crust!
you get hotter and hotter
mantle
yes it does.
the mantle
The mantle is expected to be cooler than the inner core but hotter than the outer core. The inner core is the hottest layer of the Earth, while the outer core is composed of molten iron and nickel. The mantle, located between the crust and core, experiences convection currents due to heat from the core, making it warmer than the outer core but cooler than the inner core.
the area of of earths crust that is the thickest is the mantle.
the area of of earths crust that is the thickest is the mantle.
Heat transfer in the Earth's mantle drives the movement of the Earth's crust through the process of convection. As mantle material heats up, it becomes less dense and rises, causing the overlying crust to move. At the same time, cooler mantle material sinks back down, completing the cycle of heat transfer and driving the continuous motion of tectonic plates.