The Earth's crust, mantle, and core are layers that are classified based on their compositional and physical properties.
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Compositional Properties:
- Crust: The outermost layer, composed primarily of silicate rocks. It includes continental crust (mostly granite) and oceanic crust (mostly basalt).
- Mantle: Located beneath the crust, the mantle is made up of silicate minerals that are rich in magnesium and iron (e.g., peridotite).
- Core: The innermost layer, consisting mainly of iron and nickel. It is divided into a solid inner core and a liquid outer core.
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Physical Properties:
- Crust: The crust is relatively thin and rigid compared to the other layers.
- Mantle: The mantle is much thicker and behaves like a solid but can flow slowly over geological timescales due to convection.
- Core: The outer core is in a liquid state due to the high temperatures, while the inner core is solid due to immense pressure despite also being at very high temperatures.
These layers play a crucial role in Earth's geology and geodynamics, including plate tectonics and the generation of the Earth's magnetic field.