Diastrophism Results of plate tectonics 1 volcanism 2
- Slides: 36
Diastrophism Results of plate tectonics: 1. volcanism 2. diastrophism 3. earthquakes
diastrophism: n Deformation of crust due to tectonic stress: • Folding (bending) • Faulting (breaking and displacement)
Types of Stress and Strain (Stress is force acting on rock; strain is rock’s response to stress) n Compression (shortening) n Extension (stretching)
EXTENSION COMPRESSION
Folding n Compressional stress causes rocks to buckle and fold • Anticline: arch-shaped fold • Syncline: sink-shaped fold
n Anticlines begin as ridges ; synclines begin as valleys.
n Differential erosion leads to: • Anticlinal ridges and valleys • Synclinal ridges and valleys n Differential erosion: less-resistant types of rock strata will weather and erode more rapidly than more-resistant rock strata
Anticlinal mountain/ridge Synclinal valley
What’s this? Synclinal mountain/ridge
Faulting n 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 move • Fault scarp: cliff formed along fault face
Fault from Hebgen Lake, Montana earthquake, 1959 What’s this? Fault scarp
Types of Faults 1. Normal Fault: from extensional stress Vertical movement along an inclined fault plane
normal
Horst and Graben (result of normal faulting) Horst : upfaulted block Graben: downfaulted block
Block mountains
2. Reverse Fault from compressional stress Vertical movement along inclined fault plane such that one side rides up over the other. often creates landslides
reverse
reverse
reverse
3. Overthrust fault n n Reverse fault with very low angle More horizontal than vertical movement
overthrust
3. Transcurrent (Strike-slip) Fault horizontal movement no fault scarp
Transcurrent
Transcurrent HEY! Who moved my wood pile? !@*
Transcurrent
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- Evidence of the theory of plate tectonics
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