There are differences in chemistry (the mantle is mainly ultramafic rock--the outer core is metallic), in phase (the mantle is predominately solid--the outer core is liquid), in depth (the outer core is closer to the center of the Earth), and in density (the outer core is more dense).
Mohorovicic discontinuity is located between the upper mantle and the crust, while the Gutenberg discontinuityis located between the lower mantle and the outer core.
The Earth's outer core is thicker than the mantle. The outer core is about 2,260 kilometers thick, while the mantle is approximately 2,900 kilometers thick.
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 boundary separating the Earth's mantle and core is known as the core-mantle boundary. This boundary is characterized by a sharp decrease in seismic wave velocities, indicating a difference in composition and properties between the outer core and the lower mantle.
Yes, the lower mantle is also known as the mesosphere. It is the region of Earth's mantle that lies between the upper mantle and the outer core.
Between the outer core and the crust.
outer core
Mohorovicic discontinuity is located between the upper mantle and the crust, while the Gutenberg discontinuityis located between the lower mantle and the outer core.
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 layer of hot solid material between the Earth's crust and outer core is called the mantle. It is composed of silicate rocks and is divided into the upper mantle and lower mantle. Heat from the Earth's core causes convection currents in the mantle, which drive the movement of tectonic plates.
Between the thin rocky crust and inner core, in order from upper to lower, are the upper mantle, mantle, and outer core.
The Earth's outer core is thicker than the mantle. The outer core is about 2,260 kilometers thick, while the mantle is approximately 2,900 kilometers thick.
Between the inner core and lowwer mantle.
The Crust, Mantle, Outer Core, and the Inner 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.
The distance from the outer core to the mantle is approximately 2,900 kilometers. The outer core is a layer beneath the Earth's mantle, composed mainly of iron and nickel, while the mantle is the layer located between the crust and the outer core.
The boundary separating the Earth's mantle and core is known as the core-mantle boundary. This boundary is characterized by a sharp decrease in seismic wave velocities, indicating a difference in composition and properties between the outer core and the lower mantle.