Transistion zone.
convection currents
From thick to thin: mantle, outer core, inner core, crust.
the mantle then the outer core then the inner core
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 core of the earth is surrounded by the mantle.The earth's core is called the inner core. Just outside that is the outer core, and it is liquid. Outside the liquid outer core is the mantle.
true.
convection currents
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.
From thick to thin: mantle, outer core, inner core, crust.
Starting from the core, here is a list of how to get to the surface (crust): core (middle), mantle (biggest), crust (surface, ground, rock)
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.
crust mantle core
the Gutenberg discontinuity
no! it can be in the mantle or the outer core
the mantle then the outer core then the inner core
core is a thing ...... also it can be part of the earth's surface inner core,outer core,mantle,crust
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.