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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.
The softer layer below the lithosphere is the asthenosphere. The asthenosphere begins at a depth of approximately 150 km. It has convection currents that arise from the heating and subsequent rising of material from the lower asthenosphere. These convection currents drive the movement of lithospheric plates at the surface, and are the cause of tectonic activity.
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.
Lithosphere.
30 degrees Celsius for each kilometer of depth near Earth's surface
lithosphere refers to the rocks of the earths surface and upper mantle or depth of plates. hope that helped
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.
On the Earth's surface, the depth is between 8-64 kilometers.
The Earth's lithosphere can vary in depth from 5 km at the ocean ridges to 200 km underneath mountain ranges.
temperature increases with depth
The softer layer below the lithosphere is the asthenosphere. The asthenosphere begins at a depth of approximately 150 km. It has convection currents that arise from the heating and subsequent rising of material from the lower asthenosphere. These convection currents drive the movement of lithospheric plates at the surface, and are the cause of tectonic activity.
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.
50km
The lithosphere can be 8 km to about 65km in depth.
its apparent depth is 1.5m.
100km
Both temperature and pressure increase with depth.