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Learn about different types of faults including normal and reverse faults, as well as strike-slip faults like the San Andreas Fault. Discover how folded mountains and fault-block mountains are formed due to tectonic plate movements, and understand concepts such as uplift, subsidence, and tectonic letdown.
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What is a FAULT? When rock layers BREAKwhen stress is applied One block of rock slides relative to another
Narrow base block of angled crust What is the hanging wall, see page 114 Broad base block of angled crust the foot wall?
What is a normal fault? When the hanging wall moves down relative to the footwall Occurs when tectonic forces cause tensionthat pull the blocks of rock apart
What is a REVERSE FAULT? When the Hanging wall moves up relative to the footwall Occurs when tectonic forces push the blocks of rock together (Compression)
What are STRIKE-SLIP FAULTS? Form when opposing forces cause rock to break and move horizontally Example: California’s San Andreas fault
A strike slip fault Geologic Activity, http://www.nps.gov/pore/naturescience/geologicactivity.htm
Mountain Building • Occurs because of tectonic plate movement
What are folded mountains? Form at convergent plate boundaries Rock layers that are squeezed together Make the highest mountains in the world
Folded mountain Layers that are squeezed together
What are some examples of folded mountains? Appalachian mountains The Alps Himalayan Mountains
What are fault block mountains? Tension causes large blocks of rock to drop down Example: Teton Mountains, Wyoming
Fault block mountains Grand Tetons Wyoming
What is uplift and subsidence? Subsidence—the sinking of a region of the Earth’s crust Uplift—the rising of a region of the Earth’s crust
What is Tectonic Letdown? Sinking of a region of Earth due to tension Rift zone – a set of deep cracks that form between two plates that are pulling apart
Formation of a Rift ValleySequence showing how movements deep under the Earth's Crust help to create a Rift Valley