Comparing the Layers of Earth S6E5.a.. Earth’s layers are compared by: Temperature Density –(the...

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Comparing the Layers of Earth S6E5.a.

Transcript of Comparing the Layers of Earth S6E5.a.. Earth’s layers are compared by: Temperature Density –(the...

Page 1: Comparing the Layers of Earth S6E5.a.. Earth’s layers are compared by: Temperature Density –(the thickness or depth of the layer) Composition –What each.

Comparing the

Layers of Earth

S6E5.a.

Page 2: Comparing the Layers of Earth S6E5.a.. Earth’s layers are compared by: Temperature Density –(the thickness or depth of the layer) Composition –What each.

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

Page 3: Comparing the Layers of Earth S6E5.a.. Earth’s layers are compared by: Temperature Density –(the thickness or depth of the layer) Composition –What each.

Which is the outermost layer?

THE CRUST

Temperature:

Temp of the air outside to 1600 °F

Density: 5km – 70km thick

Page 4: Comparing the Layers of Earth S6E5.a.. Earth’s layers are compared by: Temperature Density –(the thickness or depth of the layer) Composition –What each.

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

Page 5: Comparing the Layers of Earth S6E5.a.. Earth’s layers are compared by: Temperature Density –(the thickness or depth of the layer) Composition –What each.

What do you find on Earth’s crust?

• Rocks

• Mountains

• Soil

• Water

• What else???

Page 6: Comparing the Layers of Earth S6E5.a.. Earth’s layers are compared by: Temperature Density –(the thickness or depth of the layer) Composition –What each.

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.

Page 7: Comparing the Layers of Earth S6E5.a.. Earth’s layers are compared by: Temperature Density –(the thickness or depth of the layer) Composition –What each.

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!

Page 8: Comparing the Layers of Earth S6E5.a.. Earth’s layers are compared by: Temperature Density –(the thickness or depth of the layer) Composition –What each.

The Mantle• Made of 3 distinct

areas:

–Lithosphere

–Asthenosphere

–Lower Mantle

Page 9: Comparing the Layers of Earth S6E5.a.. Earth’s layers are compared by: Temperature Density –(the thickness or depth of the layer) Composition –What each.

Mantle’s Lithosphere• Density =

approx 100 km

• Composition:

–Rigid layer

–Rocky like Crust

–“Lithos” means “Stone”

• Unique? Made up by part of the Crust!

Page 10: Comparing the Layers of Earth S6E5.a.. Earth’s layers are compared by: Temperature Density –(the thickness or depth of the layer) Composition –What each.

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.

Page 11: Comparing the Layers of Earth S6E5.a.. Earth’s layers are compared by: Temperature Density –(the thickness or depth of the layer) Composition –What each.

Lower Mantle• Density = 2467 km

• Composition:– Solid

Unique? Semi-rigid

Page 12: Comparing the Layers of Earth S6E5.a.. Earth’s layers are compared by: Temperature Density –(the thickness or depth of the layer) Composition –What each.

Where the Mantle ends and the Outer Core begins is an area

called the GUTENBERG DISCONTINUITY

Gutenberg Discontinuity

Page 13: Comparing the Layers of Earth S6E5.a.. Earth’s layers are compared by: Temperature Density –(the thickness or depth of the layer) Composition –What each.

Outer Core

• Temperature = 6700 °F to 7800 °F

• Density = 2266 km

• Composition:– Liquid, Molten Metal

(Fe & Ni)

Page 14: Comparing the Layers of Earth S6E5.a.. Earth’s layers are compared by: Temperature Density –(the thickness or depth of the layer) Composition –What each.

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

Page 15: Comparing the Layers of Earth S6E5.a.. Earth’s layers are compared by: Temperature Density –(the thickness or depth of the layer) Composition –What each.

Inner Core• Temperature = 7800 °F to

13000 °F

HOTTEST LAYER!!!

• Density = 1216 km

• Composition:– Dense, solid metal ball of Fe & Ni!

Page 16: Comparing the Layers of Earth S6E5.a.. Earth’s layers are compared by: Temperature Density –(the thickness or depth of the layer) Composition –What each.

What’s unique about the Inner Core?

• Extreme pressure squeezes the atoms of the Fe & Ni so much, they cannot spread out!

• Stays solid!