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Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

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Page 1: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

Inside Earth: Chapter 1- Plate Tectonics

Section 1: Earth’s Interior

Page 2: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

What caused a 2.5 square kilometer landmass to form in the ocean off the coast of Iceland in 1963?

• An erupting volcano underneath the ocean caused an island form and to continually to grow in size for many years

Page 3: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

What did the Icelanders name this landmass? Who did they name it after?

• Icelanders named their new landmass Surtsey the god of fire

Page 5: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

The Science of Geology

Page 6: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

A scientist who studies the forces that make and shape planet Earth are called ______.

• geologists

Page 7: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

Geologists study the _____ and _____ characteristics of ______, the material that forms the surface of Earth.

• Chemical • Physical • Rock

Page 8: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

Geologists divide the forces that change the earth’s surface into two groups: _____ _____ & _____ _____.

• Constructive forces

• Destructive forces

Page 9: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

The force that builds up mountains and other landforms is known as a ______.

• Constructive Force

Page 10: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

The force that slowly wears away at mountains and eventually, every other feature on the surface of Earth is known as a _____ force. • Destructive force

Page 11: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

List some other examples of this type of a constructive force.

• Islands from volcanoes• Flooding-fertile soil• Weather-rain

Page 12: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

List some examples of this type of destructive force.

• Ocean waves• Weathering&erosion• Earthquakes

Page 13: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

Continent

• A Landmass that is surrounded by water on all sides

• Earth has seven continents

Page 14: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

Figure 2: Observing – What are the geologists in each picture doing?

• The geologist in the top picture are studying the characteristics of a cave

• The geologist in the bottom picture is investigating rock layers

Page 15: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

Geologists examine the layers of Earth to answer what three questions?

• How old is Earth?

• How has Earth’s surface changed over time?

• Why are there oceans, and how did they form?

Page 16: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

Checkpoint: What kind of indirect evidence do geologists use to study the structure of Earth?

• Geologists record seismic waves and study how they travel through Earth

Page 17: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

Guide For Reading: What does a geologist do? • Geologists study the processes

that create Earth’s features and search for clues about Earth’s history.

Page 18: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

A Journey to the Center of the Earth

Page 19: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

Describe the features of a vehicle that would be needed to travel to the center of Earth.

• A drill• A pressure detecting device• A temperature detecting device • A device that detects composition

Page 20: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

Describe the temperature change that takes place as the depth inside Earth increases.

• Rock near the surface would be cool

• About 20 meters down the rock gets warmer

• For every 40 meters that descends a temperature increases 1°C

Page 21: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

The force pushing on a surface or area is known as _______.

• Pressure

Page 22: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

Why does the pressure increase as you go deeper into Earth?

• The pressure increases as you go deeper inside the earth because amount and weight of the rock increases

Page 23: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

Figure 4: Comparing & Contrasting – How is the water in the swimming pool similar to Earth’s interior? How is it different?

• The deeper the water in the pool, the greater the pressure, just as pressure is greater the deeper you go beneath the surface of Earth

• The water in the pool does not have layers

Page 24: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

Guide For Reading: What are the main layers of Earth’s surface?

• The three main layers make up Earth’s interior:

• The crust• The mantle• The core

• Each layer has its own conditions and materials

Page 25: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

The oceanic crust is made of _____, a dark, dense rock with fine texture.

• Basalt

Page 26: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

The continental crust is made of ______, which is made of larger crystals, is less dense and is lighter in color.

• Granite

Page 27: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

Figure 5: Comparing & Contrasting-Which rock looks as if it’s made up of one material? of Several materials?

• The basalt looks like it’s made of one material

• The granite looks like it’s made of several materials.

Page 28: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior
Page 29: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

Earth’s Magnetic Field

Page 30: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

Figure 7: Relating Cause & Effect – If you shifted the magnet beneath the paper, what would happen to the iron filings?

• The iron filings would move with the magnet, again forming the same pattern above the magnet’s new position.

Page 31: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

What happens in Earth’s interior to produce Earth’s magnetic field?

• Currents in the liquid outer core force the solid inner core to spin

• Like a planet within a planet, the inner core spins inside Earth at a slightly faster rate than the rest of the planet

Page 32: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

Sharpen Your SkillsCreating Data TablesImagine that you have invented a super-strong vehicle that can resist extremely high pressure as it bores a tunnel deep into Earth’s interior. You stop several times on your trip to collect data using devices located on your vehicle’s outer hull. To see what conditions you would find at various depths on your journey, refer to Exploring Earth’s Interior on pages 22-23. Complete the table below.

Depth Name of Layer

Composition

20 km

100 km

2,000 km

4,000 km

6,000 km

Page 33: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

Sharpen Your SkillsCreating Data TablesImagine that you have invented a super-strong vehicle that can resist extremely high pressure as it bores a tunnel deep into Earth’s interior. You stop several times on your trip to collect data using devices located on your vehicle’s outer hull. To see what conditions you would find at various depths on your journey, refer to Exploring Earth’s Interior on pages 22-23. Complete the table below.

Depth Name of Layer

Composition

20 km crust

100 km

2,000 km

4,000 km

6,000 km

Page 34: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

Sharpen Your SkillsCreating Data TablesImagine that you have invented a super-strong vehicle that can resist extremely high pressure as it bores a tunnel deep into Earth’s interior. You stop several times on your trip to collect data using devices located on your vehicle’s outer hull. To see what conditions you would find at various depths on your journey, refer to Exploring Earth’s Interior on pages 22-23. Complete the table below.

Depth Name of Layer

Composition

20 km crust Solid rock, mainly granite

and basalt

100 km

2,000 km

4,000 km

6,000 km

Page 35: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

Sharpen Your SkillsCreating Data TablesImagine that you have invented a super-strong vehicle that can resist extremely high pressure as it bores a tunnel deep into Earth’s interior. You stop several times on your trip to collect data using devices located on your vehicle’s outer hull. To see what conditions you would find at various depths on your journey, refer to Exploring Earth’s Interior on pages 22-23. Complete the table below.

Depth Name of Layer

Composition

20 km crust Solid rock, mainly granite

and basalt

100 km mantle

2,000 km

4,000 km

6,000 km

Page 36: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

Sharpen Your SkillsCreating Data TablesImagine that you have invented a super-strong vehicle that can resist extremely high pressure as it bores a tunnel deep into Earth’s interior. You stop several times on your trip to collect data using devices located on your vehicle’s outer hull. To see what conditions you would find at various depths on your journey, refer to Exploring Earth’s Interior on pages 22-23. Complete the table below.

Depth Name of Layer

Composition

20 km crust Solid rock, mainly granite

and basalt

100 km mantle Solid rock

2,000 km

4,000 km

6,000 km

Page 37: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

Sharpen Your SkillsCreating Data TablesImagine that you have invented a super-strong vehicle that can resist extremely high pressure as it bores a tunnel deep into Earth’s interior. You stop several times on your trip to collect data using devices located on your vehicle’s outer hull. To see what conditions you would find at various depths on your journey, refer to Exploring Earth’s Interior on pages 22-23. Complete the table below.

Depth Name of Layer

Composition

20 km crust Solid rock, mainly granite

and basalt

100 km mantle Solid rock

2,000 km mantle

4,000 km

6,000 km

Page 38: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

Sharpen Your SkillsCreating Data TablesImagine that you have invented a super-strong vehicle that can resist extremely high pressure as it bores a tunnel deep into Earth’s interior. You stop several times on your trip to collect data using devices located on your vehicle’s outer hull. To see what conditions you would find at various depths on your journey, refer to Exploring Earth’s Interior on pages 22-23. Complete the table below.

Depth Name of Layer

Composition

20 km crust Solid rock, mainly granite

and basalt

100 km mantle Solid rock

2,000 km mantle Solid or molten material

4,000 km

6,000 km

Page 39: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

Sharpen Your SkillsCreating Data TablesImagine that you have invented a super-strong vehicle that can resist extremely high pressure as it bores a tunnel deep into Earth’s interior. You stop several times on your trip to collect data using devices located on your vehicle’s outer hull. To see what conditions you would find at various depths on your journey, refer to Exploring Earth’s Interior on pages 22-23. Complete the table below.

Depth Name of Layer

Composition

20 km crust Solid rock, mainly granite

and basalt

100 km mantle Solid rock

2,000 km mantle Solid or molten material

4,000 km Outer core

6,000 km

Page 40: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

Sharpen Your SkillsCreating Data TablesImagine that you have invented a super-strong vehicle that can resist extremely high pressure as it bores a tunnel deep into Earth’s interior. You stop several times on your trip to collect data using devices located on your vehicle’s outer hull. To see what conditions you would find at various depths on your journey, refer to Exploring Earth’s Interior on pages 22-23. Complete the table below.

Depth Name of Layer

Composition

20 km crust Solid rock, mainly granite

and basalt

100 km mantle Solid rock

2,000 km mantle Solid or molten material

4,000 km Outer core Molten iron & nickel

6,000 km

Page 41: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

Sharpen Your SkillsCreating Data TablesImagine that you have invented a super-strong vehicle that can resist extremely high pressure as it bores a tunnel deep into Earth’s interior. You stop several times on your trip to collect data using devices located on your vehicle’s outer hull. To see what conditions you would find at various depths on your journey, refer to Exploring Earth’s Interior on pages 22-23. Complete the table below.

Depth Name of Layer

Composition

20 km crust Solid rock, mainly granite

and basalt

100 km mantle Solid rock

2,000 km mantle Solid or molten material

4,000 km Outer core Molten iron & nickel

6,000 km Inner core

Page 42: Inside Earth: Chapter 1- Plate Tectonics Section 1: Earth’s Interior

Sharpen Your SkillsCreating Data TablesImagine that you have invented a super-strong vehicle that can resist extremely high pressure as it bores a tunnel deep into Earth’s interior. You stop several times on your trip to collect data using devices located on your vehicle’s outer hull. To see what conditions you would find at various depths on your journey, refer to Exploring Earth’s Interior on pages 22-23. Complete the table below.

Depth Name of Layer

Composition

20 km crust Solid rock, mainly granite

and basalt

100 km mantle Solid rock

2,000 km mantle Solid or molten material

4,000 km Outer core Molten iron & nickel

6,000 km Inner core Solid iron & nickel