Yes. The asthenosphere is molten and plastic, the lithosphere is mostly not molten and is rigid.
The lithosphere is thinner than the asthenosphere. The former is around 100 km in thickness while the latter is around 180 km in thickness.
yes it is. the aesthenosphere holds up the lithosphere
No. The asthenosphere is hotter. The deeper you go, the hotter it gets.
As odd as it is to think of things this way, continental lithosphere is more buoyant than oceanic lithosphere. The oceanic lithosphere is more dense.
The plates are part of the crust, the upper layer of the Earth. The plates are moved by currents in the upper mantle. The plates and flexible upper mantle are referred to collectively as the lithosphere and sit atop the mantle layer called the aesthenosphere.
The zone below the lithosphere is the mantle. Convection currents occur here because of the magnetism in the Earth. It is somewhat plastic like.
It is stronger.
lava is stronger
The Lithosphere Floats on top of the asthenosphere because it is less dense.
Magma moves under the lithosphere because the aesthenosphere (and magma) are ductile - they act as a fluid, although a very viscous one, and they do flow. The viscosity of a magma depends on its mineral composition. Magma will move in convection currents throughout the aesthenosphere due to the heating and cooling of it as it travels throughout the aesthenosphere.
I think you mean Lithosphere. the lithosphere is the top solid crust portion of planet Earth. it consists of the Ocean floor and Continents. Below the lithosphere is the aesthenosphere. Which begins to get very hot.
As odd as it is to think of things this way, continental lithosphere is more buoyant than oceanic lithosphere. The oceanic lithosphere is more dense.
Aesthenosphere
No continental lithosphere contains more felsic rocks than oceanic lithosphere.
The asthenosphere is more dense than the lithosphere.
As odd as it is to think of things this way, continental lithosphere is more buoyant than oceanic lithosphere. The oceanic lithosphere is more dense.
As odd as it is to think of things this way, continental lithosphere is more buoyant than oceanic lithosphere. The oceanic lithosphere is more dense.
Yes. The Lithosphere tends to fail in a brittle rather than ductile fashion.
The largest part of the lithosphere is the atmospshere
The density of the continental (granitic) lithosphere is lower than oceanic (basaltic) lithosphere. Consequently, due to buoyancy, the continental crust rides above the oceanic lithosphere and thus is not subducted. However, it is thought that pieces of the continental lithosphere break off and are subducted along with the oceanic lithosphere.