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Published byEzra Bennett Modified over 9 years ago
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Earthquakes - The movement of the ground, caused by waves of energy released as rocks move along faults Fault – a large fracture in rocks, from several meters to many kilometers long, where rocks not only crack but also move along either side of the break Types of Stresses; tension, compression, & shear Types of Faults; Normal, Reverse, Strike-Slip Types of Faults; Normal, Reverse, Strike-Slip
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1. Normal Fault – a pull apart fracture in rocks, where rocks that are above the fault surface drop downward in relation to rocks that are below the fault surface
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2. Reverse Fault – a compression fracture in rocks, where rocks that are above the fault surface are forced up over rocks that are below the fault surface
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3. Strike-Slip Fault – a break in rocks where rocks on either side of the fault move past each other, instead of above or below each other
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Concept of ‘hanging wall’ and ‘footwall’ Footwall: Rock surface ABOVE the fault Headwall: Rock surface ABOVE the fault
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Earthquakes (cont.) Slow steady pressure produces folds Types of folds; anticlines - upward bulging fold (ant hill) syncline - downward bulging fold (dip) monocline - rock layers on one side of a fold are higher than the other side
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Anticline Syncline Monocline
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Route 23 fold
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Stresses Building Mountains 1.Folded Mountains – caused by compression 2.Fault-Block Mountains – caused by tension 3.Plutonic Mountains – result from vertical force created by rising magma 4.Volcanic Mountains – result of magma from convergent boundaries reaching Earth’s surface
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Folded Mountains Fault-Block Mountains
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Plutonic Mountain – Half Dome Volcanic Mountain – Mt. Fuji
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Earthquake Evidence Creep – very slow down-slope movement, ~1cm/yr., leads to severe cracks in buildings Slide – rapid down-slope movement of soil, rocks & debris Scarps – cliff created by sudden earth movements along a fault, identified by a curved scar in the landscape Fissure – a long crack in soil or rock, up to many kilometers in length Tsunami – an ocean wave caused by earthquakes, may reach over 100ft. In height
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Scarp Creep Landslide
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Fissure Tsunami created by 9.0 earthquake on Dec.26, 2004 off the west coast of Sumatra in the Indian Ocean
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Chile Quake Feb. 27, 2010 Magnitude 8.8 Offshore Maule, Chile Resultant Tsunami
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Earthquake Damage Depends on; 1. location of earthquake 2. type of ground under buildings 3. building design & materials 4. closeness to coastline in case of tsunami
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The End
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Extra Credit Find and read a news article on Earthquakes - write a three paragraph essay about the article (at least-5 sentences per paragraph). Please include the article. Sneak it to me no later than the day of the Earthquake test for credit
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