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 is the top layer we live on, followed by the mantle and then the core.
Isostacy refers to an equilibrium level maintained by the earths crust on top of the mantle. The theory holds that the weight of the earths crust will displace a certain amount of the underlying mantle, and that an equilibrium is reached whereby the mass of the displaced crust and the mass of the displaced mantle are equal, thus holding that part of the crust at a certain height.
im pretty sure it earths crust and core or if not the top part of the mantle and the crust above it this is the only infomation i could get sorry
The outer core is composed of molten iron and nickel, which is much denser than the material that composes the mantle. So, in a sense, the mantle floats on top of the core just as the crust floats on top of the mantle.
Yes the crust and the top layer of the mantle is called Lithosphere.
The very top of Earth's mantle is known as the lithosphere. It is a rigid layer that consists of both the uppermost part of the mantle and the crust above it. The lithosphere is broken into tectonic plates that float on the semi-fluid asthenosphere beneath it.
The top part of it is made up of the crust and we are standing on it. Below the crust is the mantle followed by the core which can BURN you up into a billion pieces. But it is the gravity from the centre of Earth that holds you to the crust of Earth
The top part of the mantle and the crust above it form into lithosphere.
Yes, the crust is the top layer. It continually changes.
The Earth's crust and the uppermost part of the mantle together form the lithosphere. The lithosphere is a rigid outer layer of the Earth that is divided into tectonic plates which float on the semi-fluid asthenosphere beneath them.
The Earth's tectonic plates lay on top of the outer layer of the mantle. This layer is known as the asthenosphere.
The Earth's lithosphere is made up of the crust and the uppermost part of the mantle. It is divided into several large and small tectonic plates that float on the semi-fluid asthenosphere below. These plates interact at plate boundaries, where geological activities like earthquakes and volcanic eruptions occur.