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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
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.– Some rocks can become brittle and snap– Some rocks can bend slowly
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.
What are the 3 Types of Stress?2. Compression: squeezes rock until it folds or breaks.–Occurs where 2 plates
are colliding.
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.
Kinds of Faults• Fault – a break in the crust where rock surfaces slip
past each other.– Most faults occur along plate boundaries.
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
Normal Fault at Death Valley,
California
http://geotripper.blogspot.com/2008_02_01_archive.html
Kinds of Faults2. Reverse Faults: caused by compression– Same structure as normal fault, but rock moves in
opposite direction– Hanging wall slides upward
Animation
http://rst.gsfc.nasa.gov/Sect2/Sect2_7.html
Kinds of Faults3. Strike-Slip Faults: plates move past each other sideways• Caused by shearing formed at transform boundaries
Animation
http://comp.uark.edu/~sboss/ex4s02answers.htm
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
Anticline-syncline pair in Silurian strata, Newfoundland, New Jersey.
http://www.rci.rutgers.edu/~schlisch/structureslides/rte23folds.html
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
Basin and Range
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