lithosphere
We speak of the Earth as consisting of three main regions; the crust as the solid outermost part, the inner core at the very center and the mantle in between. Then we give the regions where they come together names and we also subdivide the three main regions and give the subdivisions names.It is the lithosphere and the asthenosphere that are the parts of the surface moving when we talk of continental drift.The lithosphere is outer portion of the Earth. It is composed of the oceanic and continental crust, along with the rigid upper mantle.The asthenosphere is the plastic like upper mantle directly below the lithosphere where rock can move, bend, and deform without breaking. Below that, the mantle become more fluid and is the major part of the volume of the Earth.The inner most part, the core, is only about 15% of the whole Earth.
The lithosphere is the hard rocky outer shell of the Earth, composed of the crust and uppermost mantle, that extends from the surface to a depth of up to 200 km at its deepest point.
Lithosphere.
The mantle extends to the core-mantle interface at approximately 2900 km depth. Thus, the mantle contains the lower portion of the lithosphere, the asthenosphere, and the mesosphere. The crust is made of the upper portion of the lithosphere.
The lithosphere can be 8 km to about 65km in depth.
The Earth's lithosphere can vary in depth from 5 km at the ocean ridges to 200 km underneath mountain ranges.
lithosphere
The lithosphere includes the Earth's crust and uppermost mantle. Oceanic lithosphere is typically about 50-100 km thick, while continental lithosphere has a range in thickness from about 40 km to perhaps 200 km.
Most resources comes from or are found within the top surface layer of the earth, which is just a few km's in depth and consists of the crust and lithosphere (especially the uppermost part of the lithosphere).
the upper part of the mantle is called the lithosphere. this layer also includes the crust.
We speak of the Earth as consisting of three main regions; the crust as the solid outermost part, the inner core at the very center and the mantle in between. Then we give the regions where they come together names and we also subdivide the three main regions and give the subdivisions names.It is the lithosphere and the asthenosphere that are the parts of the surface moving when we talk of continental drift.The lithosphere is outer portion of the Earth. It is composed of the oceanic and continental crust, along with the rigid upper mantle.The asthenosphere is the plastic like upper mantle directly below the lithosphere where rock can move, bend, and deform without breaking. Below that, the mantle become more fluid and is the major part of the volume of the Earth.The inner most part, the core, is only about 15% of the whole Earth.
The asthenosphere begins at around 100-150 km depth in the Earth. This is below the lithosphere, which consists of the crust and the uppermost mantle (the plates in plate tectonics).The asthenosphere is in the mantle, but it is still unclear how much of the mantle (which goes down to a depth of ~2900 km) is actually part of the asthenosphere.
The lithosphere is the hard rocky outer shell of the Earth, composed of the crust and uppermost mantle, that extends from the surface to a depth of up to 200 km at its deepest point.
Lithosphere.
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.
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.