crust in motion chapter 5, section 1 monday, january 25, 2010 pages 144-153

12
Crust in Motion Chapter 5, Section 1 Monday, January 25, 2010 Pages 144-153

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Page 1: Crust in Motion Chapter 5, Section 1 Monday, January 25, 2010 Pages 144-153

Crust in MotionChapter 5, Section 1

Monday, January 25, 2010

Pages 144-153

Page 2: Crust in Motion Chapter 5, Section 1 Monday, January 25, 2010 Pages 144-153

Objectives

Understand how stress forces affect rock.Describe why faults form and learn where

they occur.Learn how movement along faults change

Earth’s surface.

Page 3: Crust in Motion Chapter 5, Section 1 Monday, January 25, 2010 Pages 144-153

Vocabulary Words

Earthquake Stress Deformation Shearing Tension Compression Fault Strike-slip fault Normal fault

Hanging wall Footwall Reverse fault Fault-block mountain Fold Anticline Syncline Plateau

Page 4: Crust in Motion Chapter 5, Section 1 Monday, January 25, 2010 Pages 144-153

What is an Earthquake?

An earthquake is the shaking and trembling that results from the movement of rock beneath Earth’s surface.

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Page 5: Crust in Motion Chapter 5, Section 1 Monday, January 25, 2010 Pages 144-153

Earthquake -- cont’d

Powerful forces cause the Earth’s plates to squeeze rocks together and pull it in different directions.

This type of force is called stress.Stress adds energy to rocks.

When this stored up energy changes the shape of rocks or breaks the crust, it is called deformation.

Page 6: Crust in Motion Chapter 5, Section 1 Monday, January 25, 2010 Pages 144-153

Types of Stress Causing Deformation

There are three kinds of stress that cause deformation: Shearing: pushes a mass of rock in two opposite

directions. Tension: pulls on the crust and stretches the rock. Compression: squeezes the rock until it folds or breaks.

Shearing, tension, compression work over millions of years to change the shape and volume of rock.

Page 7: Crust in Motion Chapter 5, Section 1 Monday, January 25, 2010 Pages 144-153

Types of Faults

There are three types of faults: Strike-slip fault: rocks

on either side of the fault slide past each other sideways with little up or down motion.

Caused by shearing.

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Page 8: Crust in Motion Chapter 5, Section 1 Monday, January 25, 2010 Pages 144-153

Types of Faults -- cont’d

Normal fault: one block of rock lies above the fault while the other block lies below it. The block above is

called the hanging wall and the block below it is called the footwall.

Normal faults are caused by tension.

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Page 9: Crust in Motion Chapter 5, Section 1 Monday, January 25, 2010 Pages 144-153

Types of Faults -- cont’d

Reverse Faults: the hanging wall slides upward past the footwall. Reverse faults are

caused by compression.

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Page 10: Crust in Motion Chapter 5, Section 1 Monday, January 25, 2010 Pages 144-153

Movement Along the Fault

The amount of movement depends on how much friction there is between them. Low friction means the

blocks slide constantly without sticking.

High friction is when the blocks lock together.

When the amount of stress is greater than the amount of friction, the blocks will suddenly unlock and cause an earthquake.

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Page 11: Crust in Motion Chapter 5, Section 1 Monday, January 25, 2010 Pages 144-153

Fault-Block Mountain

Formed when normal faults uplift a block of rock.

A fold is a bend in rock that forms when compression shortens and thickens part of the crust. A fold that bends upward in an arch is an anticline. A fold that bends downward in the middle to form a

bowl is a syncline. A plateau is formed when a fault pushes up a large

flat block of rock. A plateau is a large area of the flat land elevated high

above sea level.

Page 12: Crust in Motion Chapter 5, Section 1 Monday, January 25, 2010 Pages 144-153

Homework

Workbook 5.1 (1/27)Vocabulary quiz 5.1 (1/27)