Chapter 15 4 Deforming the Earths Crust stress

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Chapter 15. 4 Deforming the Earth’s Crust

Chapter 15. 4 Deforming the Earth’s Crust

stress • a force that acts on rock deforming it’s shape or volume

stress • a force that acts on rock deforming it’s shape or volume

3 types of stress shearing tension compression pushes rock in opposite directions pulls on

3 types of stress shearing tension compression pushes rock in opposite directions pulls on crust stretches rock so that it becomes thinner in the middle squeezes rock until it folds or breaks You. Tube video-Bill Nye Stress

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

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

Folding • fold-bend in rock that forms when compression shortens & thickens part of

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

Three Types of Folds • Anticline • Syncline • Monocline

Three Types of Folds • Anticline • Syncline • Monocline

Anticline • fold in rock layers that forms an Arch

Anticline • fold in rock layers that forms an Arch

Syncline • fold in rock layers that bends down to form a bowl –

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

Anticline & syncline

Anticline & syncline

Anticline & syncline

Anticline & syncline

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

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

3 types of faults strike-slip normal reverse caused by shearing caused by tension caused

3 types of faults strike-slip normal reverse caused by shearing caused by tension caused by compression

Hanging Wall/Footwall

Hanging Wall/Footwall

Normal fault hanging wall moves down relative to the footwall hanging wall

Normal fault hanging wall moves down relative to the footwall hanging wall

Normal Faults

Normal Faults

Reverse fault hanging wall moves up relative to the footwall hanging wall

Reverse fault hanging wall moves up relative to the footwall hanging wall

Reverse Fault

Reverse Fault

Strike-Slip Fault • Faulting at a transform boundary – fault blocks slide past each

Strike-Slip Fault • Faulting at a transform boundary – fault blocks slide past each other

What kind of fault is this? strike-slip fault

What kind of fault is this? strike-slip fault

Example of a strike-slip fault San Andreas fault

Example of a strike-slip fault San Andreas fault

Fault-Block Mountains • mountains formed when normal faults cause large blocks of rocks to

Fault-Block Mountains • mountains formed when normal faults cause large blocks of rocks to slip down due to tension Grand Teton mountain range

fault-block mountain

fault-block mountain

Uplift and Subsidence • Vertical movements in the crust are divided into two types—

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)

plateau= plateau large area of flat land elevated high above sea level (an area

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

 • The Colorado Plateau is a 150, 000 square mile region covering parts

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

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

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

syncline

syncline

syncline

syncline

fold What is a bend in rock that forms when compression shortens & thickens

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

A fold is a bend in rock that forms when compression shortens & thickens

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

A fold is a bend in rock that forms when compression shortens & thickens

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

fault-block mountain • What is a mountain formed when normal faults cause a block

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

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

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

 • In a _______ fault, the rocks on either side of the fault

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

 • In a strike-slip fault, the rocks on either side of the fault

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

What are the 3 types of stress ? shearing tension compression

What are the 3 types of stress ? shearing tension compression

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

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

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

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

tension What type of stress pulls on the crust, stretching the rock so that

tension What type of stress pulls on the crust, stretching the rock so that it becomes thinner in the middle ?

 • What type of stress pushes rock in opposite directions? A. B. tension

• What type of stress pushes rock in opposite directions? A. B. tension shearing

What are the 3 types of faults? 1. strike-slip 2. normal 3. reverse

What are the 3 types of faults? 1. strike-slip 2. normal 3. reverse

What type of fault is caused by shearing? A. B. C. D. Strike-slip Normal

What type of fault is caused by shearing? A. B. C. D. Strike-slip Normal Reverse Fault-block