Crust
The Gutenberg discontinuity is found directly above the outer core.
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.
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.
mantle is the inner earth layer between the core and crust. it is separated from the crust by the layer known as Mohorovicic discontinuity or simply Moho. this layer was discovered by the seismologist known as Dr. Andria Mohorovicic in 1909 when he was studying about earth-quakes in Balkan region. Upper mantle combines with the crust to form lithosphere. The mantle is about 5000 degrees centigrades and 2900km deep. hence its hot and semi-molten stated.
the layer (of the earth) that contains the most water vapor is the troposphere
Andriza Mohorovicic discovered the Mohorovicic discontinuity popularly known as Moho It is the boundary between the crust and the mantle it is about 2,880 kilometers thick. it is the thickest part of the earth's layer
Andrija_Mohorovičić (1857-1936) was a Croatian seismologist and meteorologist who theorized the boundary layer between the Earth's crust and its mantle, now known as the Mohorovicic Discontinuity (aka Moho).
Andrija_Mohorovičić (1857-1936) was a Croatian seismologist and meteorologist who theorized the boundary layer between the Earth's crust and its mantle, now known as the Mohorovicic Discontinuity (aka Moho).
The Moho , short for Mohorovicic discontinuity , is about 7 kilometers below the floor of the ocean and the MANTLE is the layer immediately beneath the Moho !
Andrija_Mohorovičić, a Croatian seismologist (1857-1936), first theorized the boundary layer between the Earth's crust and its mantle, now known as the Mohorovicic Discontinuity (aka Moho). The layer was identified by changes in the propagation of waves generated by seismic events.
The boundary between the crust and the mantle is called the Mohorovicic discontinuity. It is also called simply the Moho and it is the abrupt divide between faster and slower speeds where the mantle starts.
The Gutenberg discontinuity is found directly above the outer core.
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.
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.
mantle is the inner earth layer between the core and crust. it is separated from the crust by the layer known as Mohorovicic discontinuity or simply Moho. this layer was discovered by the seismologist known as Dr. Andria Mohorovicic in 1909 when he was studying about earth-quakes in Balkan region. Upper mantle combines with the crust to form lithosphere. The mantle is about 5000 degrees centigrades and 2900km deep. hence its hot and semi-molten stated.
The D" layer (pronounced D double prime layer) forms the base of the Earth's lower mantle. Below this lies the outer core. This boundary zone is marked by a seismic discontinuity known as the Gutenberg discontinuity.
The D" layer (pronounced D double prime layer) forms the base of the Earth's lower mantle. Below this lies the outer core. This boundary zone is marked by a seismic discontinuity known as the Gutenberg discontinuity.