The same about the lithosphere and the core is they both are hot :-(
New lithosphere is constantly being produced at the oceanic ridges. Lithosphere is consumed at the subduction zones. A balance is maintained because older, denser proportions of oceanic lithosphere descend into the mantle at a rate equal to seafloor production.
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.
because they are all the same lakibhjfvb v dcefkeuwgvjedv'gfd
The boundary between the asthenosphere and the lithosphere is normally below the Moho (which marks the boundary between the crust and the mantle). The exception to this is below mid-ocean ridges where the moho and the lithosphere / asthenosphere boundary are at the same depth.
The same about the lithosphere and the core is they both are hot :-(
the lithosphere and the crust of the earth are the same lithosphere is another word for crust so the thickest is both of them.
The lithosphere is made up of the crust and the upper mantle. On average the lithosphere extends about 100 km into the Earth's interior.
"Lithosphere" is the term given to the rocky outer layers of the Earth. The "Earth's Crust" is another name for the same thing.
The lithosphere is made up of the crust and the upper mantle. On average the lithosphere extends about 100 km into the Earth's interior.
It is different because they are not the same
No. The lithosphere is the outermost crust, the geosphere is the inside of earth. (I think, but I know that the last person to answer said "yes" so this is a better answer.) no: you're both wrong. the lithosphere is part of the mantle, which are plate tectonics. the geosphere and lithosphere are the same thing. they are both part of earth and have to do with its interior
Hydrosphere erodes a part of lithosphere and at the same time the atmosphere is constantly incorporating a part of hydrosphere via evaporation and dumping some of it in lithosphere. From the lithosphere, it is transported back to the hydrosphere and the cycle continues.
No the lithosphere is not the same all over the world.
New lithosphere is constantly being produced at the oceanic ridges. Lithosphere is consumed at the subduction zones. A balance is maintained because older, denser proportions of oceanic lithosphere descend into the mantle at a rate equal to seafloor production.
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.
because they are all the same lakibhjfvb v dcefkeuwgvjedv'gfd