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Comparing the Layers of Earth

Comparing the Layers of Earth. S6E5.a. Earth’s layers are compared by:. Temperature Density (the thickness or depth of the layer) Composition What each layer is made of or how it is described. Which is the outermost layer?. THE CRUST Temperature: Temp of the air outside to 1598 ° F

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Comparing the Layers of Earth

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  1. Comparing the Layers of Earth S6E5.a.

  2. Earth’s layers are compared by: • Temperature • Density • (the thickness or depth of the layer) • Composition • What each layer is made of or how it is described

  3. Which is the outermost layer? THE CRUST Temperature: Temp of the air outside to 1598 °F Density: 5km – 70km thick

  4. The Crust: What’s it made of? • 2 types of crust: • Oceanic – mostly basalt rocks The thinnest crust • Continental – mostly granite rocks The thicker crust

  5. What do you find on Earth’s crust? • Rocks • Mountains • Soil • Water • What else???

  6. Where the Crust ends and the Mantle begins is an area called the MOHO Discontinuity. 1909: Andrija Mohorovicic discovers the moho discontinuity, which is the boundary between Earth’s crust and mantle.

  7. Next is the Mantle… • Mantle Temperature range: From 1598 °F to 6692 °F • Density of the WHOLE Mantle = 2867 km! • Let’s break it apart!

  8. The Mantle • Made of 3 distinct areas: • Lithosphere • Asthenosphere • Lower Mantle

  9. Mantle’s Lithosphere • Density = approx 100 km • Composition: • Rigid layer • Rocky like Crust • “Lithos” means “Stone” • Unique? Made up by part of the Crust!

  10. Mantle’s Asthenosphere • Density = 300 km • Composition: • Plastic-like • Solid, but soft • “Asthenes” means “weak” • Unique? Makes the plates move! Because it’s slowly flowing.

  11. Lower Mantle • Density = 2467 km • Composition: • Solid Unique? Semi-rigid

  12. Where the Mantle ends and the Outer Core begins is an area called the GUTENBERG DISCONTINUITY  Gutenberg Discontinuity

  13. Outer Core • Temperature = 6693 °F to 7772 °F • Density = 2266 km • Composition: • Liquid, Molten Metal (Fe & Ni)

  14. What makes the Outer Core unique? • Creates Earth’s magnetic field • High temps from the formation of the planet keep the Iron (Fe) & Nickel (Ni) liquid

  15. Inner Core • Temperature = 7772 °F to 12992 °F HOTTEST LAYER!!! • Density = 1216 km • Composition: • Dense, solid metal ball of Fe & Ni!

  16. What’s unique about the Inner Core? • Extreme pressure squeezes the atoms of the Fe & Ni so much, they cannot spread out! • Stays solid!

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