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Let’s look at the Earth
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The Inside of the Earth is made of Several Layers
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The Inside of the Earth is made of Several Layers
The Crust: A Thin Rock Material
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The Inside of the Earth is made of Several Layers
The Mantle: A Dense and Mostly Solid Rock Material
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The Inside of the Earth is made of Several Layers
The Outer Core: Liquid Iron and Nickel
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The Inside of the Earth is made of Several Layers
The Inner Core: Solid Iron and Nickel
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How Do We Know This? The Crust: The Mantle: The Outer Core:
A Thin Rock Material The Mantle: A Dense and Mostly Solid Rock Material The Outer Core: Liquid Iron and Nickel The Inner Core: Solid Iron and Nickel
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Why do the layers of the earth float on one another?
Density!!!!!
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Density determines a layer’s location!
Why does any layer float? Why does any layer sink? It is less dense than the one under it! It is more dense than the one above it!
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Density
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The Density of Earth is 5.53 gm/cm3
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The Density of Earth is 5.53 gm/cm3
We know the surface of the Earth is covered with Rocks
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The Density of Earth is 5.53 gm/cm3
The Land is covered mostly by a type of rock called Granite (density of Granite = 2.6 gm/cm3)
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The Density of Earth is 5.53 gm/cm3
The Land is covered mostly by a type of rock called Granite (density of Granite = 2.6 gm/cm3) The Ocean is mostly covered by a type of rock called Basalt (density of Granite = 3.3 gm/cm3)
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The Density of Earth is 5.53 gm/cm3
Granite = 2.7 gm/cm3 Basalt = 3.3 gm/cm3 Neither of these Rocks is dense enough to account for the density of the Earth
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The Density of Earth is 5.53 gm/cm3
Granite = 2.7 gm/cm3 Basalt = 3.3 gm/cm3 Iron has a density of 7.9 gm/cm3
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The Density of Earth is 5.53 gm/cm3
Granite = 2.7 gm/cm3 Basalt = 3.3 gm/cm3 Iron has a density of 7.9 gm/cm3 So we believe the inside of the Earth is made of a heavy element such as Iron or Nickel (density of Nickel = 8.9 gm/cm3)
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The Density of Earth is 5.53 gm/cm3
Density of Rocks 3 gm/cm3
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The Density of Earth is 5.53 gm/cm3
Density of Rocks 3 gm/cm3 Density of Iron/Nickel 8 gm/cm3
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Earth's Interior Structure
Average density Crust Mantle Core 5.5 g/cm3 3 g/cm3 5 g/cm3 11 g/cm3
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Density increases with depth !
Earth must have been molten once, allowing denser material to sink, as it started to cool and solidify.
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The Density of Earth is 5.53 gm/cm3
Density of Rocks 3 gm/cm3 Density of Iron/Nickel 8 gm/cm3 So we believe about ½ the Earth is a Rock-like material and the other ½ a heavy metal such as iron and nickel The density of the Earth will be the average of the two:
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