In general, the temperature decreases towards the surface.
The Earth's interior is divided into layers based on composition and physical properties. The outermost layer is the crust, followed by the mantle, outer core, and inner core. These layers vary in temperature, density, and state of matter, with the crust being solid, the mantle partially molten, and the outer core and inner core being mostly liquid and solid, respectively.
Scientists study seismic waves to learn about the temperature inside the Earth's crust. By analyzing the speed and direction of these waves as they travel through different layers of the Earth, scientists can infer information about the temperature and composition of the Earth's crust.
Based on temperature differences.
The Earth's layers have varying temperatures. The outermost layer, the crust, has temperatures that range from below freezing to over 1,000 degrees Fahrenheit. The inner core is the hottest layer, with temperatures reaching up to 9,000 degrees Fahrenheit.
The Earth's crust is the outermost layer of the Earth, and it is the thinnest layer compared to the mantle and core. It is divided into oceanic crust, which is thinner and denser, and continental crust, which is thicker and less dense.
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The Crust has the most oxygen in it
Crust, mantle, and core
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Crust, mantle, and core
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