Yes. That is what the asthenosphere is.
Magma could be found occurring in the lithosphere or the asthenosphere, usually originating in the asthenosphere.
There is no layer of the Earth that is made of Magma (molten rock). There is a layer called the Mohorovicic Discontinuity (or Moho) which is the boundary between the Earth's lower crust and upper mantle. The asthenosphere is a mechanically weak ductily-deforming region of the upper mantle which lies below the Moho. The asthenosphere is thought to be the source of some magma but it is not a complete layer of molten rock.
asthenosphere
Magma rises from the asthenosphere to the surface of the Earth. After it reaches temperature upward to 1000 degrees Fahrenheit, the magma starts to rise. Gases also aid in pushing the magma toward the surface, along with the tremendous pressure from the depth at which it originates.
Ridge push, slab pull, and convection.
Yes. That is what the asthenosphere is.
Yes. That is what the asthenosphere is.
Magma could be found occurring in the lithosphere or the asthenosphere, usually originating in the asthenosphere.
Magma could be found occurring in the lithosphere or the asthenosphere, usually originating in the asthenosphere.
Magma chambers
There is no layer of the Earth that is made of Magma (molten rock). There is a layer called the Mohorovicic Discontinuity (or Moho) which is the boundary between the Earth's lower crust and upper mantle. The asthenosphere is a mechanically weak ductily-deforming region of the upper mantle which lies below the Moho. The asthenosphere is thought to be the source of some magma but it is not a complete layer of molten rock.
the role of asthenosphere in magma generetion
contains hot molten rocks or magma
asthenosphere
magma chambers and volcanic conduits
Magma rises from the asthenosphere to the surface of the Earth. After it reaches temperature upward to 1000 degrees Fahrenheit, the magma starts to rise. Gases also aid in pushing the magma toward the surface, along with the tremendous pressure from the depth at which it originates.
Huge magma chambers grow under the earth and cannot be released through volcanic activity, until the pressure is too much and the magma pushes out through the earth's crust.