The Mohorovičić discontinuity (commonly shortened to Moho).
The Gutenberg Discontinuity is found above the earth layer called the outer core. This boundary line, which separates the outer core from the lower mantle, is approximately 1798 miles below the Earth's surface.
The destructive boundary where the sea floor is destroyed is called a subduction zone. In this type of boundary, one tectonic plate is forced beneath another plate, causing the oceanic crust to be destroyed as it moves into the Earth's mantle. This process can lead to the formation of deep oceanic trenches and volcanic arcs.
No, although a large part of the mantle forms the mesosphere, the upper brittle mantle is part of the lithosphere and the ductile layer of the mantle below this is formed of the asthenosphere. The mantle below the asthenosphere (i.e. that part from 700 km down to the core-mantle boundary is the mesosphere).
The crust and uppermost hard rocky mantle, together, is known as the lithosphere, which is above the plastic-like upper mantle area known as the asthenosphere.
The boundary between the troposphere and stratosphere is called the tropopause. It is characterized by a stable temperature inversion where the temperature stops decreasing with altitude and instead starts to increase. This boundary is located at an altitude of around 8-15 kilometers above the Earth's surface.
The surface feature above the mantle plume is known as the "hotspot".
The layer of the Earth above the core is called the mantle. It is located between the core and the Earth's crust. The mantle is composed of hot, semi-solid rock.
The Gutenberg Discontinuity is found above the earth layer called the outer core. This boundary line, which separates the outer core from the lower mantle, is approximately 1798 miles below the Earth's surface.
The middle mantle is just above the lower mantle.
mantle. Mantel Mantelpiece Mantelshelf
The destructive boundary where the sea floor is destroyed is called a subduction zone. In this type of boundary, one tectonic plate is forced beneath another plate, causing the oceanic crust to be destroyed as it moves into the Earth's mantle. This process can lead to the formation of deep oceanic trenches and volcanic arcs.
Tree line
Tree line
Tectonic plates that are located above mantle plumes are called hotspots. These hotspots are areas of volcanic activity that can create volcanic islands or seamounts as the tectonic plate moves over the stationary plume.
It is located in the mantle and is called Magma while in the ground and Lava when above ground.
It is located in the mantle and is called Magma while in the ground and Lava when above ground.
is the temperature if the stiffer mantle above or below its melting point