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Comparing the
Layers of Earth
S6E5.a.
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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
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Which is the outermost layer?
THE CRUST
Temperature:
Temp of the air outside to 1600 °F
Density: 5km – 70km thick
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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
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What do you find on Earth’s crust?
• Rocks
• Mountains
• Soil
• Water
• What else???
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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.
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Next is the Mantle…• Mantle Temperature range:
From 1600 °F to 6700 °F
• Density of the WHOLE Mantle = 2867 km!
–Let’s break it apart!
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The Mantle• Made of 3 distinct
areas:
–Lithosphere
–Asthenosphere
–Lower Mantle
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Mantle’s Lithosphere• Density =
approx 100 km
• Composition:
–Rigid layer
–Rocky like Crust
–“Lithos” means “Stone”
• Unique? Made up by part of the Crust!
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Mantle’s Asthenosphere• Density = 300 km
• Composition:
– Plastic-like– Solid, but softer– “Asthenes” means “weak”
– Unique? Makes the plates move! Because it’s slowly flowing.
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Lower Mantle• Density = 2467 km
• Composition:– Solid
Unique? Semi-rigid
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Where the Mantle ends and the Outer Core begins is an area
called the GUTENBERG DISCONTINUITY
Gutenberg Discontinuity
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Outer Core
• Temperature = 6700 °F to 7800 °F
• Density = 2266 km
• Composition:– Liquid, Molten Metal
(Fe & Ni)
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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
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Inner Core• Temperature = 7800 °F to
13000 °F
HOTTEST LAYER!!!
• Density = 1216 km
• Composition:– Dense, solid metal ball of Fe & Ni!
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What’s unique about the Inner Core?
• Extreme pressure squeezes the atoms of the Fe & Ni so much, they cannot spread out!
• Stays solid!