Oceanic lithosphere is dense enough to be forced down into the mantle. Continental lithosphere is not.
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 density of Earth's lithosphere is 2.5 gm/cm^3
The same about the lithosphere and the core is they both are hot :-(
The lithosphere is composed of oceanic crust (mostly basalt)
Old lithosphere is recycled back into the Earth's mantle through the process of subduction. As tectonic plates converge, one plate is forced beneath the other and descends into the mantle along a subduction zone. This process allows the old lithosphere to be recycled and remelted into the mantle, contributing to the movements and dynamics of Earth's tectonic plates.
The lithosphere is being consumed at tectonic plate boundaries through subduction zones. In these areas, one tectonic plate is forced beneath another into the Earth's mantle, eventually being melted and recycled. This process helps drive the movement of tectonic plates and shapes the Earth's surface.
no
The uppermost mantle and the crust makes the lithosphere.
The lithosphere is composed of the crust and uppermost hard, brittle mantle.
The lithosphere continuously changes due to processes such as plate tectonics, which involve the movement and interaction of Earth's tectonic plates. These movements cause the lithosphere to undergo various changes, like the formation of mountains, earthquakes, and the creation of new crust at mid-ocean ridges. Erosion and weathering also contribute to the ongoing transformation of the lithosphere.
Lithosphere (apex)
The crust and the upper mantle are a geological part of the earth called the lithosphere. There are 2 parts of the lithosphere: the oceanic lithosphere, which is made up of land underneath water, and the continental lithosphere, which is the the part made of just land. The lithosphere lies on top of the asthenosphere. The lithosphere is made up of tectonic plates, which are pieces of land floating on the lithosphere.
Oceanic lithosphere is dense enough to be forced down into the mantle. Continental lithosphere is not.
whats an antonyms for 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.