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Unit 4: Earthquakes & Volcanoes AIM: How does stress in the crust change Earth’s surface?

Unit 4: Earthquakes & Volcanoes

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Unit 4: Earthquakes & Volcanoes. AIM: How does stress in the crust change Earth’s surface?. Forces in Earth’s Crust. The movement of Earth’s plates creates enormous forces that squeeze or pull the rock in the crust. Stress – a force that acts on a rock to change its shape or volume. - PowerPoint PPT Presentation

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Page 1: Unit 4: Earthquakes & Volcanoes

Unit 4: Earthquakes & Volcanoes

AIM: How does stress in the crust change Earth’s surface?

Page 2: Unit 4: Earthquakes & Volcanoes

Forces in Earth’s Crust• The movement of Earth’s plates creates enormous

forces that squeeze or pull the rock in the crust.

• Stress – a force that acts on a rock to change its shape or volume.– Some rocks can become brittle and snap– Some rocks can bend slowly

Page 3: Unit 4: Earthquakes & Volcanoes

What are the 3 Types of Stress?• Tension, compression, and

shearing work over millions of years to change the shape and volume of rock.

1. Tension: stretches rock so it becomes thinner–Occurs where 2 plates

are moving apart.

Page 4: Unit 4: Earthquakes & Volcanoes

What are the 3 Types of Stress?2. Compression: squeezes rock until it folds or breaks.–Occurs where 2 plates

are colliding.

Page 5: Unit 4: Earthquakes & Volcanoes

What are the 3 Types of Stress?3. Shearing: pushes a mass of rock in two opposite directions–Can cause rock to break

and slip apart, or change its shape.

Page 6: Unit 4: Earthquakes & Volcanoes

Kinds of Faults• Fault – a break in the crust where rock surfaces slip

past each other.– Most faults occur along plate boundaries.

Page 7: Unit 4: Earthquakes & Volcanoes

Kinds of Faults1. Normal Faults: tension pulls crust apart – divergent• Fault is at an angle:–1 block of rock lies above – hanging wall–the other lies below – footwall

• Hanging wall slips downward

Animation

Page 8: Unit 4: Earthquakes & Volcanoes

Normal Fault at Death Valley,

California

http://geotripper.blogspot.com/2008_02_01_archive.html

Page 10: Unit 4: Earthquakes & Volcanoes

http://rst.gsfc.nasa.gov/Sect2/Sect2_7.html

Page 12: Unit 4: Earthquakes & Volcanoes

http://comp.uark.edu/~sboss/ex4s02answers.htm

Page 13: Unit 4: Earthquakes & Volcanoes

Changing Earth’s Surface1. Folding – rock bends without breaking– Upward folds – anticline– Downward folds – syncline

• Colliding plates can compress and fold crust over wide area– Produces largest mountain ranges– Ex: Himalayas in Asia

“Folding” Video Clip

Page 14: Unit 4: Earthquakes & Volcanoes

Anticline-syncline pair in Silurian strata, Newfoundland, New Jersey.

http://www.rci.rutgers.edu/~schlisch/structureslides/rte23folds.html

Page 15: Unit 4: Earthquakes & Volcanoes

Small-scale folding in stepping stones

Page 16: Unit 4: Earthquakes & Volcanoes

2. Stretching Earth’s Crust - two normal faults cut into rock– Parallel formation creates fault-block mountains

Changing Earth’s Surface

Fault-Block mountains Video Clip

Page 17: Unit 4: Earthquakes & Volcanoes

Basin and Range

Page 18: Unit 4: Earthquakes & Volcanoes

3. Uplifting forces can raise plateaus– Large area of FLAT land elevated high above sea level– Forces in crust push up large, flat blocks of rock

Changing Earth’s Surface

Plateau near Zion National Park, Utah