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Explore Earth's four layers - inner core, outer core, mantle, and crust - uncovering their composition, temperature, and unique characteristics. Delve deep into the structure of our planet, from the solid iron core to the molten outer core and rocky crust.
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Unit 2E B Plates of Earth
Earth is shaped like a ball and is made up of four layers. It is about 8,000 miles in diameter
Layers of Earth At the very center of Earth is the inner core
Vocabulary Inner core The center of Earth that is about 800 miles thick and made of solid iron and nickel
The inner core is very hot, about 9,0000 F Although it is hot enough to melt, the inner core is solid because it is under so much pressure from the layers above
The molecules of iron and nickel cannot spread out enough to become liquid Iron Nickel
Iron and nickel causing magnetic fields (blue are movements inward and yellow are movements outward)
The outer core is about 1,400 miles thick Vocabulary: Outer core The layer of Earth is outside the inner core and made of hot liquid metal
The temperature of the outer core ranges from 4,0000 F to 9,0000 F
Because the outer core is not under as much pressure as the inner core, the iron and nickel have melted (molten)
The mantle is the 3rd layer of the Earth Vocabulary: mantle The thickest layer of Earth that lies just below the crust
The top layer of the mantle is hot solid rock The bottom layer is liquid rock
The rocks in the mantle are made mostly of silicon, aluminum, iron, and magnesium
The crust is the 4th layer of Earth Vocabulary: crust The outer layer of Earth that makes up the continents and ocean floors
The crust is about 20 miles thick in most places But can be as little as 5 miles thick
The crust is made up of many kinds of rock, such as granite, sandstone, and marble