The asthenosphere is the layer of Earth that lies at a depth 60-150 mi (100-250 km) beneath Earth's surface.
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.
Mountains don't sink because of buoyancy. The continental crust and the rest of the lithosphere float on the asthenosphere like a boat on the water. Mountains have roots that extend down into the asthenosphere that coordinate to the mass of the mountain.
the mantel makes up the asthenosphere
The movement of liquid rock in the asthenosphere is mainly driven by convection currents, a process where hot rock rises, cools, and then sinks back down. This flow is due to the heat generated by the Earth's core, causing the asthenosphere to slowly move and deform over time.
The The crust and the uppermost layer of the mantle form the lithosphere. The asthenosphere, which is still in the upper mantle, is the next layer down.
Tectonic plate boundaries are faults that extend all the way down to the asthenosphere of the upper mantle.
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.
a region where oceanic plates sink down into the asthenosphere is called a subduction zone.
Mountains don't sink because of buoyancy. The continental crust and the rest of the lithosphere float on the asthenosphere like a boat on the water. Mountains have roots that extend down into the asthenosphere that coordinate to the mass of the mountain.
The mesosphere is made up of plenty of things. It is underneath the asthenosphere and the lower part of the mantle. The mesosphere extends from the bottom of the asthenosphere to the earth's core. give me a piture. The mesosphere also means middle.
The asthenosphere has the ability to slow down seismic waves. Is not made up of earths plates that would be the lithosphere.
asthenosphere
Direct Answer: AsthenosphereExplained Answer: Earthquake waves normally go faster with increasing depth. However, below the lithosphere, the upper mantle contains a curious layer in which earthquake waves unexpectedly slow down. Geologists call this layer the asthenosphere.
the mantel makes up the asthenosphere
Not exactly. The lithosphere is the crust and the top of the mantle (down to the asthenosphere).
Tornadoes start up in the clouds & make their way down to touch land.
The movement of liquid rock in the asthenosphere is mainly driven by convection currents, a process where hot rock rises, cools, and then sinks back down. This flow is due to the heat generated by the Earth's core, causing the asthenosphere to slowly move and deform over time.