The core, as it is mainly made up of iron and nickel.
The mantle is closer to the molten core of earth, so it is constantly heated by it. The crust is exposed to the atmosphere, which has some cooling effect, and the crust is, of course farthest from the core.
the earth freezers layers after density stratification which consists of the core, mantle, and crust
The mantle is less dense than the core but more dense than the crust.
mantle crust ocean outer core
Oceanic crust subducts under continental crust because it is denser. Continental crust's density is too low for it to be forced into the mantle.
The crust
The mantle is closer to the molten core of earth, so it is constantly heated by it. The crust is exposed to the atmosphere, which has some cooling effect, and the crust is, of course farthest from the core.
Crust, mantle, and then core.!(:
inner core
the earth freezers layers after density stratification which consists of the core, mantle, and crust
The mantle is less dense than the core but more dense than the crust.
mantle crust ocean outer core
The crust is above the mantle and the mantle is below the crust
Oceanic crust subducts under continental crust because it is denser. Continental crust's density is too low for it to be forced into the mantle.
No the Mantle seperates the crust and the outer core
Crust and the upper mantle
Oceanic crust is more dense than continental crust.