56
Chapter 15.4 Chapter 15.4 Deforming the Earth’s Deforming the Earth’s Crust Crust

Chapter 15.4 Deforming the Earth’s Crust

Embed Size (px)

DESCRIPTION

Chapter 15.4 Deforming the Earth’s Crust. stress. a force that acts on rock deforming it’s shape or volume. YouTube video-Bill Nye Stress. Stress causes rocks to either fold (bend) or fault (break). Folding. Folded Mountains. - PowerPoint PPT Presentation

Citation preview

Page 1: Chapter 15.4 Deforming the Earth’s Crust

Chapter 15.4Chapter 15.4Deforming the Earth’s CrustDeforming the Earth’s Crust

Page 2: Chapter 15.4 Deforming the Earth’s Crust

stressstress• a force that acts on rock deforming it’s

shape or volume

Page 3: Chapter 15.4 Deforming the Earth’s Crust

3 typesof stress

shearing tension compression

pushes rock in

opposite directions

pulls on cruststretches rock so that it becomes

thinner in the middle

squeezes rock until it folds

or breaks

YouTube video-Bill Nye Stress

Page 4: Chapter 15.4 Deforming the Earth’s Crust

Stress causes rocks to either fold (bend) or fault (break).

Page 5: Chapter 15.4 Deforming the Earth’s Crust

Folding

Folded Mountains

• fold-bend in rock that forms when compression shortens & thickens part of Earth’s crust –can create folded Mountains

Page 6: Chapter 15.4 Deforming the Earth’s Crust

Three Types of Folds

• Anticline

• Syncline

• Monocline

Page 7: Chapter 15.4 Deforming the Earth’s Crust

AAnticlinenticline • fold in rock layers that forms an Arch

Page 8: Chapter 15.4 Deforming the Earth’s Crust

Syncline

• fold in rock layers that bends down to form a bowl –SMILEY FACE!

Page 9: Chapter 15.4 Deforming the Earth’s Crust

Anticline & syncline

Page 10: Chapter 15.4 Deforming the Earth’s Crust

Anticline & syncline

Page 11: Chapter 15.4 Deforming the Earth’s Crust

Monocline

• Rock layers are folded so that both ends of the fold are horizontal.

Page 12: Chapter 15.4 Deforming the Earth’s Crust

3 typesof faults

strike-slip normal reverse

caused by shearing

caused bytension

caused bycompression

Page 13: Chapter 15.4 Deforming the Earth’s Crust

Hanging Wall/Footwall

Page 14: Chapter 15.4 Deforming the Earth’s Crust

Normal fault

hanging wall

footwall

hanging wall moves down relative to the footwall

Page 15: Chapter 15.4 Deforming the Earth’s Crust

Normal Faults

Page 16: Chapter 15.4 Deforming the Earth’s Crust

Reverse faulthanging wall moves up relative to the footwall

footwall

hanging wall

Page 17: Chapter 15.4 Deforming the Earth’s Crust

Reverse Fault

Page 18: Chapter 15.4 Deforming the Earth’s Crust

Strike-Slip Fault

• Faulting at a transform boundary – fault blocks slide past each other

Page 19: Chapter 15.4 Deforming the Earth’s Crust

What kind of fault is this?strike-slip fault

Page 20: Chapter 15.4 Deforming the Earth’s Crust

San Andreas fault

Example of a strike-slip fault

Page 21: Chapter 15.4 Deforming the Earth’s Crust

Fault-Block Mountains

• mountains formed when normal faults cause large blocks of rocks to slip down due to tension

Grand Teton mountain range

Page 22: Chapter 15.4 Deforming the Earth’s Crust

fault-block fault-block mountainmountain

Page 23: Chapter 15.4 Deforming the Earth’s Crust

Uplift and Subsidence• Vertical movements in the crust are

divided into two types—– Uplift – the rising of regions of the Earth’s

crust to higher elevations (mountains and rebound – slow movement back to normal level after weight is removed)

– Subsidence – sinking of regions of Earth’s crust to lower elevations (rift zones and oceanic crust as it moves away from the ridge)

Page 24: Chapter 15.4 Deforming the Earth’s Crust

plateauplateau= large area of flat land elevated high above sea level (an area of uplift)

Page 25: Chapter 15.4 Deforming the Earth’s Crust

• The Colorado Plateau is a 150,000 square mile region covering parts of Arizona, Utah, Colorado, and New Mexico.

Page 26: Chapter 15.4 Deforming the Earth’s Crust
Page 27: Chapter 15.4 Deforming the Earth’s Crust

syncline

• What is a fold in rock layers that bends down to form a bowl ?

Page 28: Chapter 15.4 Deforming the Earth’s Crust

syncline

Page 29: Chapter 15.4 Deforming the Earth’s Crust

syncline

Page 30: Chapter 15.4 Deforming the Earth’s Crust

fold

What is a bend in rock that forms when compression shortens & thickens part of Earth’s crust ?

Page 31: Chapter 15.4 Deforming the Earth’s Crust

A fold is a bend in rock that forms when compression shortens & thickens part of Earth’s crust.

Page 32: Chapter 15.4 Deforming the Earth’s Crust

A fold is a bend in rock that forms when compression shortens & thickens part of Earth’s crust.

Page 33: Chapter 15.4 Deforming the Earth’s Crust

fault-block mountain• What is a mountain formed when normal faults cause a block of rock to slip down?

Sierra-Nevada mountain range

Page 34: Chapter 15.4 Deforming the Earth’s Crust
Page 35: Chapter 15.4 Deforming the Earth’s Crust
Page 36: Chapter 15.4 Deforming the Earth’s Crust

aanticline nticline

• What is a fold in rock layers that forms an arch ?

Page 37: Chapter 15.4 Deforming the Earth’s Crust
Page 38: Chapter 15.4 Deforming the Earth’s Crust
Page 39: Chapter 15.4 Deforming the Earth’s Crust

• In a _____________

fault, the rocks on either side of the fault slip past each other sideways.

Page 40: Chapter 15.4 Deforming the Earth’s Crust

• In a strike-slip fault, the rocks on either side of the fault slip past each other sideways.

Page 41: Chapter 15.4 Deforming the Earth’s Crust
Page 42: Chapter 15.4 Deforming the Earth’s Crust

What are the 3 types

of stress ?

shearing tension compression

Page 43: Chapter 15.4 Deforming the Earth’s Crust

• The 3 types of stress are shearing, tension and compression.

Page 44: Chapter 15.4 Deforming the Earth’s Crust

• The 3 types of stress are shearing, tension and compression.

Page 45: Chapter 15.4 Deforming the Earth’s Crust

tensiontensionWhat type of stress pulls on the

crust, stretching the rock so that it becomes thinner in the middle ?

Page 46: Chapter 15.4 Deforming the Earth’s Crust
Page 47: Chapter 15.4 Deforming the Earth’s Crust
Page 48: Chapter 15.4 Deforming the Earth’s Crust

B. shearingB. shearing

• What type of stress pushes rock in opposite directions?

A. tensionA. tension

Page 49: Chapter 15.4 Deforming the Earth’s Crust
Page 50: Chapter 15.4 Deforming the Earth’s Crust
Page 51: Chapter 15.4 Deforming the Earth’s Crust

What are the 3 types of faults?What are the 3 types of faults?

1. strike-slip2. normal3. reverse

Page 52: Chapter 15.4 Deforming the Earth’s Crust
Page 53: Chapter 15.4 Deforming the Earth’s Crust
Page 54: Chapter 15.4 Deforming the Earth’s Crust

What type of fault is caused by shearing?

A.A. Strike-slipStrike-slipB.B. NormalNormalC.C. ReverseReverseD.D. Fault-blockFault-block

Page 55: Chapter 15.4 Deforming the Earth’s Crust
Page 56: Chapter 15.4 Deforming the Earth’s Crust