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Crust, mantle, and then core.!(:
The moon's average density is about the same as the density of mantle of the Earth.
The crust rides or floats on the mantle. :)
The stiffer mantle (upper) is one of the layers of the earth's crust and composed of hot liquid rock. The range of density is between 3-100 or 3.4g/cm and 4.3g/cm.
Yes
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.
inner core
Crust, mantle, and then 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.
The moon's average density is about the same as the density of mantle of the Earth.
Density will vary from place to place with ocean crust being denser than continental crust.
The core, as it is mainly made up of iron and nickel.