Layers of the Earth
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📅 2/11/2026
Introduction to Earth's Layers
The Earth is composed of several distinct layers, each with unique properties.
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The Earth's Crust
- The crust is the outermost layer, ranging from 5-70 km in thickness.
- It consists of continental crust (granite) and oceanic crust (basalt).
- The crust is where all terrestrial life and geological activity occur.
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The Mantle
- The mantle lies beneath the crust, extending about 2,900 km deep.
- It is composed of silicate rocks rich in iron and magnesium.
- Convection currents in the mantle drive plate tectonics.
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The Core: Outer & Inner
- The outer core is liquid, composed of iron and nickel, and generates Earth's magnetic field.
- The inner core is solid due to extreme pressure, despite temperatures over 5,000°C.
- Together, they are about 3,470 km in radius.
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Summary & Importance
- Earth's layers influence surface geology, climate, and magnetic field.
- Studying these layers aids in predicting natural disasters and resource exploration.
- Each layer plays a critical role in making Earth habitable.
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