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Internal Structure of The Earth Physical Layering Determining the Earth's Internal Structure C. The Earth's Internal Layered Structure and Composition D. VELOCITY AND DENSITY VARIATION WITHIN THE EARTH The immense amount of heat energy released from gravitational energy and from the decay of radioactive elements melted the entire planet, and it is still cooling off today. Denser materials like iron (Fe) sank into the core of the Earth, while lighter silicates (Si), other oxygen (O) compounds, and water rose near the surface. The earth is divided into four main layers: the inner core, outer core, mantle, and crust. The core is composed mostly of iron (Fe) and is so hot that the outer core is molten, with about 10% sulphur (S). The inner core is under such extreme pressure that it remains solid. Most of the Earth's mass is in the mantle, which is composed of iron (Fe), magnesium (Mg), aluminum (Al), silicon (Si), and oxygen (O) silicate compounds. At over 1000 degrees C, the mantle is solid but can deform slowly in a plastic manner. The crust is much thinner than any of the other layers, and is composed of the least dense potassium (K), calcium (Ca) and sodium (Na) aluminum-silicate minerals. Being relatively cold, the crust is rocky and brittle, so it can fracture in earthquakes.
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OLM Science6_6
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Chapter 6 Plate
Tectonics Inside the Earth Section 1
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Chapter 6 Plate
Tectonics Restless Continents Section 2
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Sea-floor spreading
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Chapter 6 Plate
Tectonics The theory of Plate Tectonics Section 3
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Chapter 6 Plate
Tectonics Deforming the Earth’s Crust Section 4
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Anticline
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Syncline
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Monocline
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