the mantle is the part under the crust made up of nickel and iron moving about causing volcanoes whereas the core is solid because it is so tightly packed the minerals and metals have very constricted movement. the mantle is also the largest part of the Earth. the core has 2 sections the inner core and outer core
Between the thin rocky crust and inner core, in order from upper to lower, are the upper mantle, mantle, and outer core.
The two core layers (outer and inner core) are denser and thicker than the mantle. The mantle is the layer between the core and the crust of the Earth, and it is thicker than the core layers.
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.
The mantle.
The layer of the Earth above the core is called the mantle. It is located between the core and the Earth's crust. The mantle is composed of hot, semi-solid rock.
The mantle is a layer of the Earth that lies between the core and the crust, while the core is the innermost layer made up of the outer liquid core and the solid inner core. Another difference is that the mantle is mainly composed of solid rock materials, while the core is primarily made up of metallic elements such as iron and nickel.
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).
The Earth is made up of four main layers: the crust, mantle, outer core, and inner core. The crust is the outermost layer and is solid, while the mantle is solid but capable of flowing slowly. The outer core is liquid, and the inner core is solid due to high pressure. These layers differ in composition, temperature, and physical state, but they all play a role in Earth's structure and behavior.
The boundary of mantle and core are called Gutenberg Discontinuity
The boundary between the mantle and core is called the core-mantle boundary. This region is marked by a significant change in density and composition, representing the transition from the solid mantle to the liquid outer core of the Earth.
Between the thin rocky crust and inner core, in order from upper to lower, are the upper mantle, mantle, and outer core.
The two core layers (outer and inner core) are denser and thicker than the mantle. The mantle is the layer between the core and the crust of the Earth, and it is thicker than the core layers.
The outer core.
The mantle.
The mantle.
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 Earth is made up thus: Inner core, outer core, mantle, crust. We live on the crust, with semi-plastic molten rock forming much of the mantle beneath us.