I'm stuck on it too!
this is bull shitt
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.
The asthenosphere (or low-velocity zone) is believed to be about 200 kilometers (120 miles) thick. The layers of rock that make up the asthenosphere are thought to be partially melted and hotter than those in the lithosphere. If this were true, it would explain why the asthenosphere might also have less surface integrity, making it a possible source for the generation of new magma.
The difference between the core and the lithosphere is the core is on the top of the lithosphere and the lithosphere is on the bottom of the core
lithosphere.
lithosphere is differ from the asthenophere because lithosphere in greek lithos means "stone" and asthenophere is what the crust floats on.
you make the lithosphere with the mantle and the asthenophere.
No, it is not. It is found in the lithosphere. The lithosphere is between the mantle and the crust.
The Asthenosphere is the upper layer of Earth's mantle. It lies below the Lithosphere.
the lithosphere is what the biosphere lives on and if there was no lithosphere the biosphere would die. the biosphere is what the lithosphere needs to survive. the bodies of dead matter decomposes to make the lithosphere able to make more biomatter for the biosphere.
this is bull shitt
Which two spheres interact when a glacier erodes rock
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.
the asthenophere is 85 km thick
The asthenosphere (or low-velocity zone) is believed to be about 200 kilometers (120 miles) thick. The layers of rock that make up the asthenosphere are thought to be partially melted and hotter than those in the lithosphere. If this were true, it would explain why the asthenosphere might also have less surface integrity, making it a possible source for the generation of new magma.
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 uppermost mantle and the crust makes the lithosphere.