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Chapter 6 – Earthquakes Section 1: Forces in Earth’s Crust

Chapter 6 – Earthquakes

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Chapter 6 – Earthquakes. Section 1: Forces in Earth’s Crust. Types of Stress. Stress & plate boundaries. Types of Stress. What type of landform results from tension? valley. What type of landform results from compression? mountain. Silly Putty Stress. Silly Putty. - PowerPoint PPT Presentation

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Page 1: Chapter 6 – Earthquakes

Chapter 6 – EarthquakesSection 1: Forces in Earth’s Crust

Page 2: Chapter 6 – Earthquakes

Types of Stress

Stress & plate boundaries

Page 3: Chapter 6 – Earthquakes

Types of Stress

What type of landform results from tension?valley

What type of landform results from compression?mountain

Page 4: Chapter 6 – Earthquakes

Silly PuttyStress

Page 5: Chapter 6 – Earthquakes

Silly PuttyWhich part of this activity models

the type of stress that would produce anticlines and synclines?

When we pushed the ends together – compression

Page 6: Chapter 6 – Earthquakes

Folding Earth’s Crust

Page 7: Chapter 6 – Earthquakes

Folding Earth’s Crust

Who can point out an anticline?Where is a syncline in this picture?

Page 8: Chapter 6 – Earthquakes

How can I tell the difference among the three types of faults?

Normal fault

Tension

Hanging wall moves down

Reverse fault

Compression

Hanging wall moves up

Strike-Slip fault

Shearing

Movement is side-to-side w/ very little up/down

Do hand models here.

Page 9: Chapter 6 – Earthquakes

Types of Faults What type of fault is

this?Normal faultWhat stress causes

this?tensionWhich wall moves –

the hanging wall or the footwall?

The hanging wallIn what direction?down.

Page 10: Chapter 6 – Earthquakes

Types of Faults

What type of fault is this?

reverse faultWhat stress causes

this?compressionWhich wall moves –

the hanging wall or the footwall?

The hanging wallIn what direction?Up and over the

footwall

Page 11: Chapter 6 – Earthquakes

Types of Faults

What type of fault is this?

Strike-slip faultWhat stress causes

this?shearingHow is this fault

different from the other two?

Rocks slip past each other with very little up/down movement.

Page 12: Chapter 6 – Earthquakes

Fault Block Mountains

Page 13: Chapter 6 – Earthquakes

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