Layers of the Earth Learning Objectives



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Bog'liq
Shavkatov Shaxboz Shavkatovich

Upper Mantle
Convection Currents
Middle Mantle
Lower Mantle

Core


Inner Core
Outer Core

Outer Core

  • Composition: Molten (liquid) metal that is about 4,700°C (8,500°F)
  • Thickness: 2,266 km (1,400) miles
  • State of Matter: Composed of the melted metals nickel and iron (liquid)
  • Located about 1,800 miles beneath the crust.

Inner Core

  • Solid sphere made mostly of iron and has Nickel
  • It is believed to be as hot as 6,650°C (12,000°F)
  • Heat in the core generated by the radioactive decay of uranium and other elements
  • It is solid because of the pressure from the outer core, mantle, and crust compressing it.
  • Thickness: 1271 km (800 miles)

What do these two images tell us about the layers of the Earth?

Temperature increases as depth increases

Look at the information in the graph and table below. What’s the relationship between depth and density/pressure?

Density and Pressure increase as depth increases

Add this statement to the arrow going down on your foldable.


Temperature,
Density and Pressure increases as depth increases

Which layer of the Earth has the greatest temperature, pressure, and density?


Core
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