silicon
Continental crust is less dense than oceanic crust.
The mantle is hotter than the crust.
The Mantle--The layer directly below the crust which is delineated from the crust by the Mohorovicic Discontinuity, where seismic waves increase in velocity. The division between the mantle and the crust is a chemical one, the rocks and constituent minerals being higher in magnesium and lower in silicon and aluminum than crustal rocks. The mantle comprises 84% of Earth's volume.
The Earth's crust is on the exterior, not the interior; that is why it is called the crust. It is on the outside. It is made mostly of rock, of various kinds. The rock of the crust is on average less dense than the rock of the mantle, which lies beneath the crust.
Peridotite is thought to be the dominant rock in the upper portions of the mantle. It's ultramafic, meaning it contains less than 45% silica.
The mantle has less aluminum and silicon than the crust does.
silicon
The mantle contains more iron, making it denser.the mantle contains more magnesium and less aluminum than the crust .this make sthe mantle denser than the crust.
The crust lies on top of the mantle because it is composed of less dense materials than the mantle is. The crust is essentially floating on the mantle.
the crust(~2.7g/cm3) is less dense than the mantle(~3.3 g/cm3)
the crust is lighter and less dense than the mantle...thus it floats on top.
Continental crust is less dense than oceanic crust.
less dense than the material of the Earth's mantle
Because its less dense
The crust is much thinner than the mantle.
The mantle is hotter than the crust.
The crust is much thinner than the mantle.