Earths Interior Andie


Published on

Published in: Technology, Education
1 Like
  • Be the first to comment

No Downloads
Total views
On SlideShare
From Embeds
Number of Embeds
Embeds 0
No embeds

No notes for slide

Earths Interior Andie

  1. 1. <ul><li>What does the inside of the Earth look like? </li></ul>
  2. 2. <ul><li>How do we determine the composition of the Earth? </li></ul><ul><li>Scientists cannot see the interior so they must use other ways to figure it out! </li></ul><ul><li>Earthquakes have many different types of waves </li></ul><ul><ul><li>These waves travel at different speeds through solids and liquids </li></ul></ul><ul><ul><li>Some waves don’t travel at all through liquids. </li></ul></ul><ul><li>Measuring these waves tells us what is in the Earth’s core and where the materials change. </li></ul>
  3. 4. Earth Layers <ul><li>The Earth is divided into four main layers. </li></ul><ul><ul><li>*Inner Core </li></ul></ul><ul><ul><li>*Outer Core </li></ul></ul><ul><ul><li>*Mantle </li></ul></ul><ul><ul><li>*Crust </li></ul></ul>
  4. 5. The Earth’s Crust <ul><li>The crust is the thinnest layer on Earth </li></ul><ul><li>There are two types of crust </li></ul><ul><ul><ul><li>Oceanic crust – made mostly of the igneous rock basalt. Found under the ocean. Relatively thin. </li></ul></ul></ul><ul><ul><ul><li>Continental crust – made mostly of granite. Found under the continents. Relatively thick. </li></ul></ul></ul>
  5. 6. Special parts of the Crust <ul><li>Lithosphere </li></ul><ul><ul><li>Crust is the upper part of the lithosphere </li></ul></ul><ul><ul><li>Broken up into large plates </li></ul></ul><ul><li>Asthenosphere </li></ul><ul><ul><li>Upper part of mantle, below lithosphere </li></ul></ul><ul><ul><li>130 – 160 km thick </li></ul></ul><ul><ul><li>Cooler part of the mantle that the lithospheric plates slide on top of. </li></ul></ul>
  6. 9. The Earth’s Mantle <ul><li>Located directly above the outer core </li></ul><ul><li>Starts below the crust </li></ul><ul><li>Is the largest layer </li></ul><ul><li>80% of the Earth’s volume & 68% of Earth’s mass </li></ul>
  7. 10. The Earth’s Mantle <ul><li>Composed of more iron than the crust. </li></ul><ul><li>Density, pressure, and temperature all increase the deeper you go in the mantle </li></ul><ul><li>Temperature ranges from 870 C – 2200 C </li></ul>
  8. 12. Special layers of the mantle <ul><li>Lithosphere – crust plus the upper, solid part of the mantle. Forms plates. </li></ul><ul><li>Asthenosphere – just under the lithosphere. Slow moving “Silly putty” layer on which the lithospheric plates slid. (Solid rock that flows very slowly.) </li></ul>
  9. 14. Currents in the Mantle
  10. 15. The Earth’s Core <ul><li>The Earth’s Core </li></ul><ul><li>Composed of the inner and outer core </li></ul><ul><li>Both are made of iron and nickel </li></ul>
  11. 16. <ul><li>How do scientists know that there is a solid inner core? </li></ul>
  12. 18. The Earth’s Outer Core <ul><li>The Outer Core - Liquid </li></ul><ul><li>Surrounds the inner core </li></ul><ul><li>Temperature ranges from 2200 C – 5000 C near inner core </li></ul><ul><li>Molten (liquid) iron and nickel </li></ul>
  13. 20. The Earth’s Inner Core <ul><li>The Inner Core - Solid </li></ul><ul><li>Temperature reaches 5000 C </li></ul><ul><li>Solid iron and nickel </li></ul><ul><ul><li>Usually both would be liquid but are solid in the core because of the incredible pressure </li></ul></ul><ul><li>The solid core is the source of Earth’s magnetic field </li></ul>
  14. 21. What do you know about these layers?