Earth’s Layers
Crust Outer  most layer Thinnest 5 to 100 kilometer (km) thick Temperatures range from 0°  C to 1000°C
Crust Composition:           mostly silicon, oxygen, sodium, small amounts of magnesium, potassium, and iron.
Crust       “Two Types”Continental   Crust Thickestup to 100 km at  mountains Most abundant rock is  granite
 Oceanic   Crust Asthin as 5 km Most abundant rock is basalt Density averages 3g per cm³
Crust/MantleMohorovicic Discontinuity (Moho): Transitionboundary  between the crust and  mantle
Crust/MantleMohorovicic Discontinuity (Moho): This boundary marks a  significant change in  chemical composition.
Mantle 67%  of Earth’s mass 2,900 km thick Temperature ranges from  1000° C to 3700 ° C
MantleDensity   averages from 4.3g to 5.4g per cm³Composition: mostly silicon, oxygen, magnesium, and iron
Mantle Convection   currents occur here
MantleDivided   into 3 layers: 1.   Lithosphere 2.   Asthenosphere 3.   Mesophere
Mantle Lithosphere: 10 to 300 km thick Solid and made up of crust  and mantle material VERY rigid Divided into sectio...
MantleAsthenosphere 250  km thick Soft layer that allows  plates to shift
MantleMesosphere 2550km thick Lower part of the mantle
CoreDivided  into 2 layers: 1.   Outer Core 2.   Inner Core
CoreOuter   Core Liquid 2200   km thick
CoreOuter   Core: Composition:  Iron and  Nickel, 10% sulfur and  oxygen
CoreOuter   Core: Density:   10g to 12g per  cm³ Temperature: 4000° to  5000° C
CoreInner   Core: Solid 1230  km thick About 6380 km beneath  Earth’s surface
Core Inner   Core: Composition:    Iron and  Nickel Density: 15 g per cm³ Temperature: 5000° to  6000° C
Earth’s Layers Scientistsuse indirect methods to gain information and knowledge of Earth’s interior (example: earthquakes).
Earth’s Layers Seismic  waves from earthquakes travel at different speeds depending on the density and composition of the...
Earth’s LayersScientists  are able to take this information and learn about the interior of Earth.
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Earth’s layers

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Earth’s layers

  1. 1. Earth’s Layers
  2. 2. Crust Outer most layer Thinnest 5 to 100 kilometer (km) thick Temperatures range from 0° C to 1000°C
  3. 3. Crust Composition: mostly silicon, oxygen, sodium, small amounts of magnesium, potassium, and iron.
  4. 4. Crust “Two Types”Continental Crust Thickestup to 100 km at mountains Most abundant rock is granite
  5. 5.  Oceanic Crust Asthin as 5 km Most abundant rock is basalt Density averages 3g per cm³
  6. 6. Crust/MantleMohorovicic Discontinuity (Moho): Transitionboundary between the crust and mantle
  7. 7. Crust/MantleMohorovicic Discontinuity (Moho): This boundary marks a significant change in chemical composition.
  8. 8. Mantle 67% of Earth’s mass 2,900 km thick Temperature ranges from 1000° C to 3700 ° C
  9. 9. MantleDensity averages from 4.3g to 5.4g per cm³Composition: mostly silicon, oxygen, magnesium, and iron
  10. 10. Mantle Convection currents occur here
  11. 11. MantleDivided into 3 layers: 1. Lithosphere 2. Asthenosphere 3. Mesophere
  12. 12. Mantle Lithosphere: 10 to 300 km thick Solid and made up of crust and mantle material VERY rigid Divided into sections called plates
  13. 13. MantleAsthenosphere 250 km thick Soft layer that allows plates to shift
  14. 14. MantleMesosphere 2550km thick Lower part of the mantle
  15. 15. CoreDivided into 2 layers: 1. Outer Core 2. Inner Core
  16. 16. CoreOuter Core Liquid 2200 km thick
  17. 17. CoreOuter Core: Composition: Iron and Nickel, 10% sulfur and oxygen
  18. 18. CoreOuter Core: Density: 10g to 12g per cm³ Temperature: 4000° to 5000° C
  19. 19. CoreInner Core: Solid 1230 km thick About 6380 km beneath Earth’s surface
  20. 20. Core Inner Core: Composition: Iron and Nickel Density: 15 g per cm³ Temperature: 5000° to 6000° C
  21. 21. Earth’s Layers Scientistsuse indirect methods to gain information and knowledge of Earth’s interior (example: earthquakes).
  22. 22. Earth’s Layers Seismic waves from earthquakes travel at different speeds depending on the density and composition of the ground they move through.
  23. 23. Earth’s LayersScientists are able to take this information and learn about the interior of Earth.
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