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Published byRandell Ray Modified over 9 years ago
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Deforming the Earth’s Crust
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Deformation Deformation: process by which a rock changes shape due to _______ stress
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Stress causes ________ and _________ 1. Compression: type of stress that occurs when an object is _______________ – Occurs at ____________ plate boundaries 2. ________: type of stress that occurs when rock is stretched/pulled – Occurs at __________ plate boundaries folding faulting squeezed/pushed convergent Tension divergent
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Stress 3. Shear: type of stress that occurs when objects slide past each other (rubbing) –Occurs at ___________ plate boundaries transform
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Folding Folding: the ________of rock layers due to stress 1. __________: upward arching fold 2. Syncline: __________ trough like fold 3. Monocline: both ends of fold are __________ bending Anticline downward horizontal
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1. ______________________ 2. _____________________ 3. _______________________
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1. Syncline 2. Anticline 3. Monocline
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Faulting Fault: a ________in a body of rock along which one _____slides relative to the other _____________ are common along fault lines In non-vertical faults, the fault is at an ______, which creates a _____________and ________ break block Earthquakes angle hanging wall footwall
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1. Normal Fault: the hanging wall moves _______compared to the footwall – _________stress occurs 2. __________ Fault: the hanging wall moves up compared to the footwall – _______________stress occurs down Tension Reverse Compression
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Normal and Reverse Faults A. ____________________________ B. ___________________________
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Normal and Reverse Faults A. Normal Fault B. Reverse Fault
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3. Strike-Slip Fault: the break in the rock is _______, but the rocks move __________ – Example: ______________Fault in California – Shear stress – NOTE: This type of fault does NOT create a footwall or hanging wall because the break in the rock is not at an angle vertical horizontal San Andreas
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Birds-Eye View
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San Andreas Fault
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PictureType of FaultType of StressType of Boundary
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PictureType of FaultType of StressType of Boundary Reverse Fault Strike Slip Fault Normal Fault Compression Shear Tension Convergent Transform Divergent
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Mountain Building 1. Folded Mountains: Formed at convergent plate boundaries – Highest, Smooth – Ex: Appalachian, Andes, Alps, Himalayas
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ALPS
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APPALACHIAN MOUNTAINS
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ANDES MOUNTAINS
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HIMALAYAN MOUNTAINS
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2. Fault-Block Mountains: Formed at divergent boundaries – Sharp, jagged peaks – At a fault, block of rocks drops down – Ex: Grand Tetons, Sierra Nevada
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SIERRA NEVADA MOUNTAINS
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GRAND TETON MOUNTAINS
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3. Volcanic Mountains: Formed at convergent boundaries – Eruption and cooling of magma – Creates islands – Ex: Mt. Kea, Mt. Loa, Mt. St. Helens, Mt. Pinatubo
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MT. MAUNA KEA
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MT. MAUNA LOA
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MT. PINATUBO
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MT. ST. HELEN
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