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Earth Layers
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Density Density = mass/volume
Heating an object causes it’s molecules to spread out causing it’s volume to change. Examples liquid, solid, gas phases Door key Marbles in bag
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Viscosity A material’s Resistance to flow.
How can viscosity be changed. 1. Adding Heat 2. Adding Water This will become extremely important when studying volcanoes.
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Earth’s Layers What three things increase the closer to the center of the Earth (core) we go? Density (Composition, what matter it is made up of), temperature ( It gets Hotter!!!) and pressure. What are the three main layers of the Earth? - Core, Mantle and Crust
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The Crust Made up of Silicates. (Very light material)
Averages around 40 km in thickness. The Earth’s crust is like the shell of an egg, very thin!
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The Mantle Composed of mostly silicates, but is also rich in iron and magnesium which makes it more dense than the crust. The Mantle has 3 parts Lithosphere (100km thick) Asthenosphere (100km thick) Mesosphere (2650km thick!)
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The Core Extremely Hot center of the Earth! 5500 C Two parts
Outer Core (liquid iron) 2,250km Inner Core (Solid iron due to high pressure) 1,300km
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Earth Cross Section Drawing
Drawing must include: -All layers -Crust, Mantle (lithospere, asthenosphere,and mesosphere.) Outer and Inner Core. -Each Layer must be clearly labeled with a title, the thickness of the layer and the composition of the layer. - Neatness will be taken into consideration when being graded! Drawing will be worth 25 points. Use notes!!!!!
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