nine
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.
Oceanic lithosphere is dense enough to be forced down into the mantle. Continental lithosphere is not.
Tectonic plates, 3 plates
What part in the egg is the lithosphere
20%
Mantle
More lithosphere facts:The lithosphere is the solid outer layer of the planetIt is 70-100 kilometers thickIt "floats" on top of a warmer, non-rigid layerThe temperature beneath the lithosphere can reach 1,000 degrees CelsiusThere is about 10 percent molten material at the lower portions of the lithosphere
mantle.
The lithosphere can be 8 km to about 65km in depth.
The metal that is most abundant in the lithosphere is iron. Over 5.6 percent of Earth's mass is comprised of iron.
plate tectionics theory......................:-)
nine
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.
There are two kinds of plates- continental lithosphere and oceanic lithosphere. There are many types of plate boundaries, like convergent, divergent, transform, and more. Continental lithosphere is granite and oceanic is basalt.
The uppermost mantle and the crust makes the lithosphere.
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