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Diastrophism Results of plate tectonics: 1.volcanism2.diastrophism3.earthquakes
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diastrophism: Deformation of crust due to tectonic stress: Deformation of crust due to tectonic stress: Folding (bending)Folding (bending) Faulting (breaking and displacement)Faulting (breaking and displacement)
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Types of Stress and Strain (Stress is force acting on rock; strain is rock’s response to stress) Compression (shortening) Compression (shortening) Extension (stretching) Extension (stretching)
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EXTENSION COMPRESSION
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Folding Compressional stress causes rocks to buckle and fold Compressional stress causes rocks to buckle and fold Anticline: arch-shaped foldAnticline: arch-shaped fold Syncline: sink-shaped foldSyncline: sink-shaped fold
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Anticlines begin as ridges ; synclines begin as valleys. Anticlines begin as ridges ; synclines begin as valleys.
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Differential erosion leads to: Differential erosion leads to: Anticlinal ridges and valleysAnticlinal ridges and valleys Synclinal ridges and valleysSynclinal ridges and valleys Differential erosion: less-resistant types of rock strata will weather and erode more rapidly than more-resistant rock strata Differential erosion: less-resistant types of rock strata will weather and erode more rapidly than more-resistant rock strata
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Anticlinal mountain/ridge Synclinal valley
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What’s this? Synclinal mountain/ridge
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Faulting Rock is strained beyond ability to remain intact; rock fractures; one side is displaced with respect to the other. Rock is strained beyond ability to remain intact; rock fractures; one side is displaced with respect to the other. Fault plane: surface along which 2 sides moveFault plane: surface along which 2 sides move Fault scarp: cliff formed along fault faceFault scarp: cliff formed along fault face
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Fault from Hebgen Lake, Montana earthquake, 1959 What’s this? Fault scarp
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Types of Faults 1. Normal Fault: from extensional stress Vertical movement along an inclined fault plane
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normal
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Horst and Graben (result of normal faulting) Horst : up- faulted block Graben: down- faulted block
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Block mountains
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2. Reverse Fault from compressional stress Vertical movement along inclined fault plane such that one side rides up over the other. often creates landslides
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reverse
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reverse
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reverse
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3. Overthrust fault Reverse fault with very low angle Reverse fault with very low angle More horizontal than vertical movement More horizontal than vertical movement
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overthrust
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3. Transcurrent (Strike-slip) Fault horizontal movement no fault scarp
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Transcurrent
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Transcurrent HEY! Who moved my wood pile?!@*
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Transcurrent
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San Andreas
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