The outer and inner core.
The Moho separates the crust and the mantle.
The two layers of discontinuity in Earth's interior are the Mohorovičić discontinuity (Moho) that separates the Earth's crust from the underlying mantle, and the Gutenberg discontinuity that marks the boundary between the mantle and the outer core. These discontinuities are characterized by changes in seismic wave velocity and composition.
No. The Moho (more correctly the Mohorovičić discontinuity) is the name given to a seismic discontinuity between the Earth's crust and mantle. The seismic discontinuity between the Earth's mantle and liquid core is known as the Gutenberg discontinuity or the CMB - Core Mantle Boundary.
The Gutenberg Discontinuity is a boundary within the Earth's interior that separates the outer core from the lower mantle. It is characterized by a rapid increase in seismic wave velocities, indicating a change in composition and physical properties. The Gutenberg Discontinuity is located at a depth of about 2,900 kilometers (1,800 miles) beneath the Earth's surface.
The boundary between the mantle and core was discovered by a seismologist named Inge Lehmann in 1936. She observed a reflection of seismic waves off this boundary, later named the "Lehmann discontinuity," which helped confirm the Earth's core-mantle structure.
lower mantle from upper core
No, the Lehmann discontinuity is believed to be located between 220 km and 260 km beneath the Earth's surface. The Gutenberg discontinuity, on the other hand, sits at a depth of around 2,900 km.
The Mohorovičić discontinuity (Moho) separates the Earth's crust from the underlying mantle. It is found beneath continents and beneath ocean basins.
The Moho separates the crust and the mantle.
mohorocivic discontinuity or moho
Yes. It is called the Mohorovicic Discontinuity, where seismic waves increase in velocity.
The two layers of discontinuity in Earth's interior are the Mohorovičić discontinuity (Moho) that separates the Earth's crust from the underlying mantle, and the Gutenberg discontinuity that marks the boundary between the mantle and the outer core. These discontinuities are characterized by changes in seismic wave velocity and composition.
No. The Moho (more correctly the Mohorovičić discontinuity) is the name given to a seismic discontinuity between the Earth's crust and mantle. The seismic discontinuity between the Earth's mantle and liquid core is known as the Gutenberg discontinuity or the CMB - Core Mantle Boundary.
The Gutenberg Discontinuity is a boundary within the Earth's interior that separates the outer core from the lower mantle. It is characterized by a rapid increase in seismic wave velocities, indicating a change in composition and physical properties. The Gutenberg Discontinuity is located at a depth of about 2,900 kilometers (1,800 miles) beneath the Earth's surface.
They mark the boundaries of differing layers of the Earth. The Moho marks the boundary between the crust and the mantle, whereas the Gutenberg discontinuity marks the boundary between the mantle and outer core.
The boundary between the mantle and core was discovered by a seismologist named Inge Lehmann in 1936. She observed a reflection of seismic waves off this boundary, later named the "Lehmann discontinuity," which helped confirm the Earth's core-mantle structure.
The seismic discontinuity at the base of the crust is known as the Mohorovičić discontinuity, or Moho for short. It marks the boundary between the Earth's crust and the underlying mantle, where seismic waves experience a sudden change in velocity.