The mechanically weak portion of the upper mantle of the Earth from 45-155 mi. (72-250 km) down, also called the Low Velocity Zone as its squishiness slows soundwaves from earthquakes.
The aesthenosphere, which is located in the top part of the Earth's mantle is the layer lying underneath the tectonic plates. Collective movement in these plates cause a gradual rise in the aesthenosphere, thereby resulting to land elevation.
Below your feet as you read this - unless you're on board a ship on the ocean! The Continental Crust is the foundation rock for the continents, and is usually covered to a greater of less depths by sedimentary rocks and drift deposits. In turn it floats on the Aesthenosphere, the outer layer of the Mantle.
Seismologists investigating undersea earthquakes have found that molten rock lubricates faults. This decreases the amount of friction between sides of the fault and decreases the intensity of earthquakes. They also found that the fragmentation of fault lines along the seafloor contributes an earthquake-dampening effect.+++I think you've mis-read your source. The earthquakes are undersea because they are on the subduction thrust plane between a sinking ocean-floor plate and the continent above it, under the continental shelf. The lubricant is not molten rock but wet sea-floor sediment, but the friction does help the Aesthenosphere heat partially the subducting basalt, with the water also acting a flux to help the melting.
The Earth's asthenosphere starts at depths of around 100 to 200 km below the surface and extends down to around 700 km. This is part of the upper mantle.Directly below the lithosphere. The asthenosphere is located between 100-350 km below the surface of the Earth. The Asthenosphere is a ductile yet solid layer located inthe upper mantle.in the upper mantle
Aesthenosphere
Magma moves under the lithosphere because the aesthenosphere (and magma) are ductile - they act as a fluid, although a very viscous one, and they do flow. The viscosity of a magma depends on its mineral composition. Magma will move in convection currents throughout the aesthenosphere due to the heating and cooling of it as it travels throughout the aesthenosphere.
The aesthenosphere, which is located in the top part of the Earth's mantle is the layer lying underneath the tectonic plates. Collective movement in these plates cause a gradual rise in the aesthenosphere, thereby resulting to land elevation.
The Lithosphere Floats on top of the asthenosphere because it is less dense.
In my opinion, plate tectonics, glaciers, aesthenosphere, the space shuttle's "crawler," and slugs
Yes, the aesthenosphere is the part of the upper mantle that is highly viscous and mechanically weak behaving as a ductile solid.
Yes. The asthenosphere is molten and plastic, the lithosphere is mostly not molten and is rigid.
The aesthenosphere is kept deformable largely through heat generated by radioactive decay
I think you mean Lithosphere. the lithosphere is the top solid crust portion of planet Earth. it consists of the Ocean floor and Continents. Below the lithosphere is the aesthenosphere. Which begins to get very hot.
Lithospheric plates made up of the upper mantle and crust float on the soft, flowing aesthenosphereand are moved around by the flow of the aesthenosphere caused by convection from the core.
Below your feet as you read this - unless you're on board a ship on the ocean! The Continental Crust is the foundation rock for the continents, and is usually covered to a greater of less depths by sedimentary rocks and drift deposits. In turn it floats on the Aesthenosphere, the outer layer of the Mantle.
The plates are part of the crust, the upper layer of the Earth. The plates are moved by currents in the upper mantle. The plates and flexible upper mantle are referred to collectively as the lithosphere and sit atop the mantle layer called the aesthenosphere.