convection currents
The boundary that separates the Earth's core from the mantle is known as the core-mantle boundary (CMB). It lies approximately 2,900 kilometers beneath the Earth's surface and marks the transition between the solid inner core and the molten outer core.
The boundary between the mantle and core is known as the core-mantle boundary. It lies approximately 2,900 kilometers below the Earth's surface. This boundary separates the molten iron-nickel outer core from the solid iron-nickel inner core.
The transition zone separates the upper mantle from the lower mantle in the Earth's interior. This region experiences changes in temperature and pressure, leading to distinct physical and chemical properties. Seismic waves also show variations in velocity when passing through this zone.
The Core Mantle boundary - also known as the Guttenberg discontinuity separates the earth's mantle from its core. It is divided into two layers, the inner core and the outer core. The inner core, the center of earth, is solid and about 780 miles (1,250 km) thick. The outer core is so hot that the metal is always molten, but the inner core pressures are so great that it cannot melt, even though temperatures there reach 6700ºF (3700ºC). The outer core is about 1370 miles (2,200 km) thick. Because the earth rotates, the outer core spins around the inner core and that causes the earth's magnetism.
From thick to thin: mantle, outer core, inner core, crust.
The boundary that separates the Earth's core from the mantle is known as the core-mantle boundary (CMB). It lies approximately 2,900 kilometers beneath the Earth's surface and marks the transition between the solid inner core and the molten outer core.
It is composed of very hot rock that is "plastic" (slowly moving and deforming). It is not as liquid as the outer core, or the magma that separates the crust from the mantle.
the Gutenberg discontinuity
The boundary between the mantle and core is known as the core-mantle boundary. It lies approximately 2,900 kilometers below the Earth's surface. This boundary separates the molten iron-nickel outer core from the solid iron-nickel inner core.
The boundary between the mantle and the core is called the core-mantle boundary and also The Gutenberg Discontinuity which marks the upper boundary of the D'' (D Double Prime) layer.
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 transition zone separates the upper mantle from the lower mantle in the Earth's interior. This region experiences changes in temperature and pressure, leading to distinct physical and chemical properties. Seismic waves also show variations in velocity when passing through this zone.
The Core Mantle boundary - also known as the Guttenberg discontinuity separates the earth's mantle from its core. It is divided into two layers, the inner core and the outer core. The inner core, the center of earth, is solid and about 780 miles (1,250 km) thick. The outer core is so hot that the metal is always molten, but the inner core pressures are so great that it cannot melt, even though temperatures there reach 6700ºF (3700ºC). The outer core is about 1370 miles (2,200 km) thick. Because the earth rotates, the outer core spins around the inner core and that causes the earth's magnetism.
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 core is corey and the mantle is mantely
3160 miles-mantle to inner core.
From thick to thin: mantle, outer core, inner core, crust.