The lithosphere is the rigid outer layer of the Earth, consisting of the crust and upper part of the mantle. It is also known as the Earth's geosphere or solid outer shell.
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.
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.
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 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.
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
The crust is the outermost layer of the Earth's surface, while the lithosphere includes the crust as well as the uppermost part of the mantle. In this context, the crust is part of the lithosphere. The lithosphere is composed of the crust and the rigid upper portion of the mantle and is divided into several tectonic plates.
The lithosphere is part of the Earth's crust and uppermost mantle; it includes the crust itself. So, the distance to the lithosphere is essentially the same as the thickness of the crust, which varies from about 5 to 75 kilometers (3 to 46 miles) beneath the oceans and continents.
The lithosphere and the crust are both parts of the Earth's outermost layer, but the lithosphere includes the crust and the uppermost part of the mantle. The crust is the solid, outermost layer of the Earth's surface, while the lithosphere is defined by its rigid behavior and consists of the crust and a portion of the upper mantle.
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.
Humans do not directly use the lithosphere. The lithosphere is the rigid outer layer of the Earth that includes the crust and upper mantle. While humans do not use the lithosphere in the same way we use the atmosphere or hydrosphere, we do rely on the resources contained within the lithosphere, such as minerals, metals, and fossil fuels, for economic activities and infrastructure development.
No, the lithosphere is not the same all over the world. It varies in thickness, composition, and structure due to geological activity such as plate tectonics. This results in different landscapes, topography, and geological features across the Earth's surface.
The uppermost mantle and the crust makes the lithosphere.