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Layers of the Earth Mesosphere Crust pg. 52 • Thin, but rigid top layer • Made up primarily of basalt rock (ocean) and granite rock (continents) – The oceanic crust is denser then the continental rock! • Thickness: 0-100 km Mantle • Partially molten rock that can flow • Makes up 68% of the mass of the Earth • Thickness: 3000 km thick • Divided into layers: – Lithosphere: Acts like a rigid, but still brittle solid. – Asthenosphere: Plastically (not liquid!) layer. Core • Made up of nickel and iron, which makes this layer magnetic and very dense • Thickness: 3500 km • Divided into layers – Outer Core: liquid – Inner Core: solid But wait, there’s more. . . • The Earth has layers due to density differences, above the crust, though, what do we encounter? • Gas has mass and can be confined to a volume, so is there layers to our air? – Yes, yes there is Layers of the Atmosphere pg. 55 • Troposphere: only layer that has weather, contains 90% of the mass • Stratosphere: where airplanes fly, contains the ozone layer, warm layer • Mesosphere: coldest layer (0 C to -90 C) Layers of the Atmosphere (cont) • Thermosphere: technically hot but it would feel cold to us • Exosphere: blends into space • REMEMBER: The atmosphere has layers because of density differences, just like our Earth!