The interior of Earth between a depth of 5200 kilometers and 6300 kilometers is inferred to be composed mostly of liquid iron and nickel, forming the outer core. This layer is characterized by its high temperatures and pressures, which facilitate the movement of molten metal. The dynamics of the outer core are crucial for generating Earth’s magnetic field through the geodynamo effect.
The region of the Earth's interior between the crust and the core is known as the mantle. It extends from the base of the crust down to the outer core, reaching depths of about 2,900 kilometers (1,800 miles). The mantle is composed of solid rock that behaves plastically over long periods, allowing for convection currents that drive plate tectonics. This layer plays a crucial role in the Earth's geological processes and heat transfer.
One major difference between oceanic crust and continental crust is their composition and density. Oceanic crust is primarily composed of basalt and is denser and thinner, averaging about 7 kilometers in thickness. In contrast, continental crust is mainly composed of lighter granitic rocks and is thicker, averaging around 30-50 kilometers. This difference in density contributes to the distinct characteristics of oceanic and continental tectonic plates.
The Earth's mantle is located between the outer core and the Earth's crust. It is a layer of hot, dense rock that is primarily composed of silicate minerals. The mantle makes up the bulk of the Earth's interior and plays a key role in plate tectonics and the movement of the Earth's crust.
The carbonaceous meteorites represent the mantle of the Earth. Pallesite meteorites are composed of iron and olivine which represents the transition between the core and the mantle.
The layer located between the Earth's crust and the core is called the mantle. It extends to a depth of about 2,900 kilometers below the Earth's surface and is composed of solid rock that behaves plastically over geological time. The mantle plays a crucial role in tectonic activity and the movement of the Earth's plates.
The region of the Earth's interior between the crust and the core is known as the mantle. It extends from the base of the crust down to the outer core, reaching depths of about 2,900 kilometers (1,800 miles). The mantle is composed of solid rock that behaves plastically over long periods, allowing for convection currents that drive plate tectonics. This layer plays a crucial role in the Earth's geological processes and heat transfer.
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Explicit details are directly stated in the text, while inferred details are not explicitly stated but can be pieced together by the reader through context clues and implicit information. Explicit details are clear and specific, while inferred details require interpretation and critical thinking.
the mantle is the largest layer of Earth's interior..... and a very hot one!!!!
52 kilometers.
there are 304.52 kilometers in between oslo and bergan
One major difference between oceanic crust and continental crust is their composition and density. Oceanic crust is primarily composed of basalt and is denser and thinner, averaging about 7 kilometers in thickness. In contrast, continental crust is mainly composed of lighter granitic rocks and is thicker, averaging around 30-50 kilometers. This difference in density contributes to the distinct characteristics of oceanic and continental tectonic plates.
kilometers and kilometers..
From a sample of a population, the properties of the population can be inferred.
what is the distance between the us and Australia.
The Earth's mantle is located between the outer core and the Earth's crust. It is a layer of hot, dense rock that is primarily composed of silicate minerals. The mantle makes up the bulk of the Earth's interior and plays a key role in plate tectonics and the movement of the Earth's crust.
The carbonaceous meteorites represent the mantle of the Earth. Pallesite meteorites are composed of iron and olivine which represents the transition between the core and the mantle.