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Lithosphere

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Crust contains what?

Lithosphere


Oceanic crust contains more of which three elements than the continental crust?

Oceanic crust contains more magnesium, iron, and calcium than continental crust.


Which layer of the earth contains the crust and upper mantle?

The layer of the Earth that contains both the crust and upper mantle is called the Lithosphere.


What layer of the earth contains granite and basalt in the GREATEST abundance?

The crust is the layer of the Earth that contains granite and basalt in the greatest abundance. These rocks are commonly found in the continental crust (granite) and oceanic crust (basalt).


What does the Earth's crust contains?

The Earth's crust contains a variety of minerals such as silicon, oxygen, aluminum, and iron. It also includes different types of rocks, such as granite, basalt, and sandstone. Additionally, the Earth's crust contains water in the form of groundwater and oceans.


Which layer contains the least mass?

The crust


Which layer of earth contains the athenosphere?

crust


What layer contains the tectonic plates?

the crust


The mantle is denser than the crust because it contains more what?

The mantle is denser than the crust because it contains more iron and magnesium-rich minerals. These minerals have a higher density compared to the minerals found in the crust, such as silica and aluminum.


Oceanic crust is denser than the continental crust because it contains more of which 3 elements?

It is the crust and mantle,and core


Oceanic crust is denser than the continental crust because it contains more of which three elements?

Oceanic crust is denser than continental crust because it contains more magnesium, iron, and calcium. These heavier elements contribute to the higher density of the oceanic crust compared to the continental crust.


Which earths crust contains granite?

Continental crust contains granite. This type of crust is thicker and less dense compared to oceanic crust. Granite is a common rock in the continental crust due to its formation through the cooling and solidification of magma below the Earth's surface.