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Stress in the Earth. Stress. Stress is a force that changes a rocks shape or volume Because stress is a force it adds energy to the rock. Stress. There are three types of stress occurring in the Earth’s crust: Shearing Tension Compression. Shearing.
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Stress • Stress is a force that changes a rocks shape or volume • Because stress is a force it adds energy to the rock
Stress • There are three types of stress occurring in the Earth’s crust: • Shearing • Tension • Compression
Shearing • When rock is pushed in opposite directions and the layers slide by each other.
Tension • When rock layers pull apart and stretch.
Compression • Caused when parts of the crust squeeze together.
Any change in the volume or shape of the layers is called deformation • Slow deformation of the crust causes uplift and folding (mountain ranges). • Rapid deformation of the crust results from Earthquakes
Faults • If stress builds in a rock it can break. • A fault is a break in the Earth’s crust where the rock moves.
Faults • There are three basic types of faults: • Strike-Slip (lateral) • Normal • Reverse
Strike-Slip Fault • Caused by shearing forces • Rocks on either side slide past each other.
Normal Fault • Caused by tension • The foot wall moves up relative to the hanging wall
Normal faults usually form at an angle • The block that is above the crack is called the Hanging Wall • The block that is below the crack is called the Foot Wall
Reverse Fault • Caused by compression forces • The foot wall moves down relative to the hanging wall
Reverse Fault • A special type of reverse fault is a thrust fault • In a thrust fault the hanging wall is pushed out over the foot wall