Chemistry
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.
Earths mantle is less dense and very hot. The mantle is 2885km thick.
The temperature difference between oceanic and continental crust is primarily due to variations in their thickness and composition. Oceanic crust is thinner and denser, leading to higher temperatures in the mantle beneath it. In contrast, continental crust is thicker and less dense, resulting in lower temperatures.
The layer of the Earth next to the core is called the mantle. It is a rocky layer located between the core and the Earth's crust. The mantle's composition is primarily silicate rocks.
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 upper mantle is harder than the lower mantle
The mantle is below the plates.
Compare molting and metamorphos
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.
Yes, however there is no clear boundary between crust and mantle as both are basaltic and stationary. There is a small solid iron core.
Earths mantle is less dense and very hot. The mantle is 2885km thick.
The temperature difference between oceanic and continental crust is primarily due to variations in their thickness and composition. Oceanic crust is thinner and denser, leading to higher temperatures in the mantle beneath it. In contrast, continental crust is thicker and less dense, resulting in lower temperatures.
The layer of the Earth next to the core is called the mantle. It is a rocky layer located between the core and the Earth's crust. The mantle's composition is primarily silicate rocks.
mantle
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 earths mantle is less dense and it's very hot.
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.