Transistion zone.
The mantle extends from the Earth's surface down to a depth of about 2,900 kilometers (1,800 miles). The bottom of the mantle is defined by the mantle-core boundary, which separates it from the outer core. This boundary is located at approximately 2,900 kilometers beneath the Earth's surface.
The mantle and core are separated by the Gutenberg Discontinuity, a boundary about 2,900 kilometers beneath the Earth's surface. This discontinuity marks the transition from the lower mantle to the outer core, which is composed of molten iron and nickel.
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.
From thick to thin: mantle, outer core, inner core, crust.
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 mantle and core are separated by the Gutenberg Discontinuity, a boundary about 2,900 kilometers beneath the Earth's surface. This discontinuity marks the transition from the lower mantle to the outer core, which is composed of molten iron and nickel.
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.
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.
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.
Starting from the core, here is a list of how to get to the surface (crust): core (middle), mantle (biggest), crust (surface, ground, rock)
the Gutenberg discontinuity
crust mantle core
From thick to thin: mantle, outer core, inner core, crust.
no! it can be in the mantle or the 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.
core is a thing ...... also it can be part of the earth's surface inner core,outer core,mantle,crust