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Forces in Earth’s Crust (pages 162–168)
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Forces in Earth’s Crust (pages 162–168)

Feb 23, 2016

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Forces in Earth’s Crust (pages 162–168). Key Questions What happens to rocks when they are placed under the large forces created by plate movements?. - PowerPoint PPT Presentation
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Page 1: Forces in Earth’s Crust (pages 162–168)

Forces in Earth’s Crust(pages 162–168)

Page 2: Forces in Earth’s Crust (pages 162–168)

Key Questions

What happens to rocks when they are placed under the large forces created by plate movements?

Page 3: Forces in Earth’s Crust (pages 162–168)

Types of Stress (page 163)

Key Concept:

Tension, compression, and shearing work over millions

of years to change the shape and volume of rock.

Page 4: Forces in Earth’s Crust (pages 162–168)

You should be able to…

Explain how stress in the crust changes the earth’s surface.

Describe where faults are usually found and why they form.

Page 5: Forces in Earth’s Crust (pages 162–168)

When Earth’s plates move, rocks are pushed and pulled.

The pushing and pulling forces cause:

stress.

Page 6: Forces in Earth’s Crust (pages 162–168)

Stress adds energy to rocks. Rocks keep storing the energy

until they cannot stand any more stress. Then the rocks break or

change shape.

Page 7: Forces in Earth’s Crust (pages 162–168)

Tension is stress that pulls and stretches rocks. Tension makes rocks thinner in the

middle. Tension happens when two plates move apart.

Page 8: Forces in Earth’s Crust (pages 162–168)

Compression is stress that squeezes rocks. Compression

makes rocks fold or break. Compression happens when

two plates push together.

Page 9: Forces in Earth’s Crust (pages 162–168)

Shearing is stress that pushes rocks in opposite directions.

Shearing makes rocks break, slip apart, or change shape. Shearing happens when two plates slip past each other in opposite directions.

Page 10: Forces in Earth’s Crust (pages 162–168)

Answer the following questions.

?

?

?? ???

?

?? ???

Page 11: Forces in Earth’s Crust (pages 162–168)

Circle the letter of the choice that describes how stress

affects rocks.

a. Stress adds energy to rocks.b. Stress uses up the energy in rocks.c. Stress squeezes energy out of rocks.

Page 12: Forces in Earth’s Crust (pages 162–168)

Pushes and pulls on rocks cause

Stress that makes rocks fold or break is called

stress

compression

Page 13: Forces in Earth’s Crust (pages 162–168)

Stress that stretches rocks is called

Stress that makes rocks break, slip apart, or change shape is called

tension

shearing

Page 14: Forces in Earth’s Crust (pages 162–168)

Before stress Kinds of stress After stress

a.

b.

c.

compression

tension

shearing

Page 15: Forces in Earth’s Crust (pages 162–168)

Kinds of Faults

(pages 164–165)

Page 16: Forces in Earth’s Crust (pages 162–168)

Key Concept:

Most faults occur along plate boundaries, where

the forces of plate motion push or pull the crust so

much that the crust breaks.

Page 17: Forces in Earth’s Crust (pages 162–168)

Students will be able to…

Describe where faults are usually found and why they form.

Page 18: Forces in Earth’s Crust (pages 162–168)

There are three main types of faults:

normal faults

reverse faults

strike-slip faults

Page 19: Forces in Earth’s Crust (pages 162–168)

A fault is a break in Earth’s crust where rocks are under

stress.

Page 20: Forces in Earth’s Crust (pages 162–168)

In many faults, the fault line is slanted. So the block of rock on one side of the fault is above the block

of rock on the other side of the fault.

Page 21: Forces in Earth’s Crust (pages 162–168)

The top block is called the hanging wall. The bottom block is called the footwall.

Page 22: Forces in Earth’s Crust (pages 162–168)

There are three different types of faults:

normal faults reverse faults

strike-slip faults

Each type is caused by a different kind of stress on rocks.

Page 23: Forces in Earth’s Crust (pages 162–168)

A normal fault happens when tension pulls rocks apart. In a normal fault, the hanging wall slips down and

becomes lower than the footwall.

Page 24: Forces in Earth’s Crust (pages 162–168)

A reverse fault happens when compression pushes rocks together.

In a reverse fault, the hanging wall slides up and becomes higher than

the footwall.

Page 25: Forces in Earth’s Crust (pages 162–168)

A strike-slip fault happens when shearing pushes rocks in opposite directions. In a strike-slip fault, two

blocks of rock move past each other, but neither block moves up or down.

Page 26: Forces in Earth’s Crust (pages 162–168)

Answer the following questions

? ???

?

?? ???

Page 27: Forces in Earth’s Crust (pages 162–168)

Circle the letter of the choice that explains what causes a

fault.

a. Stress increases on rocks until they move.b. Energy slowly drains away from rocks.c. Rocks heat up and melt.

Page 28: Forces in Earth’s Crust (pages 162–168)

1. Fill in the blanks in the table about faults and stresses.

Faults and Stresses

Kind of Fault Type of Stress That Causes Fault

Normal fault a.

b. compression

c. shearing

tensionReverse fault

Strike-slip fault

Page 29: Forces in Earth’s Crust (pages 162–168)

a.

1. Fill in the blanks to label the kind of fault shown in each diagram.

Hanging Footwall Footwall wall Hanging

w all

a. b.

c.

Reverse fault Normal fault

Strike-slip fault

Page 30: Forces in Earth’s Crust (pages 162–168)

Changing Earth’s Surface (pages 166–

168)

Page 31: Forces in Earth’s Crust (pages 162–168)

Key Concept:

Over millions of years, the forces of plate movement

can change a flat plain into landforms such as anticlines

and synclines, folded mountains, fault-block

mountains, and plateaus.

Page 32: Forces in Earth’s Crust (pages 162–168)

Students will be able to…

Identify the land features that result from plate movement.

Page 33: Forces in Earth’s Crust (pages 162–168)

Stresses in Earth’s crust cause the surface to change.

Different stresses cause different changes.

Page 34: Forces in Earth’s Crust (pages 162–168)

Compression causes folding. Folding is like a rug getting

wrinkled up when it is pushed across the floor.

Page 35: Forces in Earth’s Crust (pages 162–168)

Folds that bend upward into ridges are called anticlines.

Folds that bend downward into valleys are called synclines.

Page 36: Forces in Earth’s Crust (pages 162–168)

Tension causes stretching. When crust stretches, many

normal faults form.

Page 37: Forces in Earth’s Crust (pages 162–168)

Sometimes a block of rock moves upward between two

normal faults. The block forms a mountain called a fault-

block mountain.

Page 38: Forces in Earth’s Crust (pages 162–168)

Stresses in the crust can also form plateaus. A plateau is a large area of flat land that has been lifted up above sea level.

Page 39: Forces in Earth’s Crust (pages 162–168)

Answer the following questions.

? ???

?

?? ???

Page 40: Forces in Earth’s Crust (pages 162–168)

Circle the letter of the sentence that describes how a fault-block mountain forms.a. A block of rock moves upward between two normal faults.b. The crust becomes wrinkled like a rug.c. Rocks are pushed together by compression.

Page 41: Forces in Earth’s Crust (pages 162–168)

Is the following sentence true or false?

A plateau forms when flat land is pushed up above sea level.

TRUE

Page 42: Forces in Earth’s Crust (pages 162–168)

1. Circle the letter of the stress that causes Earth’s surface to look like the surface in the diagram below. a. tension b. compression c. shearing