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Earthquakes Mr. Silva
Earthquakes and Plate Tectonics• Earthquakes are vibrations of the earth’s  crust.• Usually occurs when rocks under stress...
Elastic Rebound Theory• According to the theory, the rocks on each  side of a fault are moving slowly.• If the fault is lo...
Elastic Rebound Theory• As they slip into their new position,  the rocks energy is released in form of  vibrations called ...
Elastic Rebound Theory• Where the slippage occurs is known as  the focus of the earthquake.• The point on the earth surfac...
Depths of Earthquake Focuses90% of earthquakes have a shallow focus.• Shallow-focus earthquakes have a  depth of 70km or l...
Major Earthquake Zones• Most earthquakes occur along the  edges of lithospheric plates.  – The largest zone is known as th...
Major Earthquake ZonesPacific Ring         Mid-ocean  of Fire              Ridge                            Eurasian-     ...
Fault Zones• Fault Zones are groups of interconnecting  faults that come together on a boundary.  – Example: San Andres Fa...
San Andres Fault
Review Questions1. Explain the rebound theory.2. In earthquakes that cause the   greatest damage, at what depth   would sl...
4.1 earthquakes
4.1 earthquakes
4.1 earthquakes
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4.1 earthquakes

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  • Transcript of "4.1 earthquakes"

    1. 1. Earthquakes Mr. Silva
    2. 2. Earthquakes and Plate Tectonics• Earthquakes are vibrations of the earth’s crust.• Usually occurs when rocks under stress suddenly shift along a fault.• When the stress becomes too great along a fault, rocks suddenly slip and grind past each other.• This slipping causes trembling and vibrations of an earthquake.
    3. 3. Elastic Rebound Theory• According to the theory, the rocks on each side of a fault are moving slowly.• If the fault is locked, stress in the rocks increases.• When the stress reaches a certain point, the rocks react by – fracturing, – separating at their weak point – Springing back to their original shape – Or rebound
    4. 4. Elastic Rebound Theory• As they slip into their new position, the rocks energy is released in form of vibrations called seismic waves.• The release of this stress, often increase stress in other rocks along the fault, causing them to fracture and spring back.• This reaction is the reason that many earthquakes have aftershocks.
    5. 5. Elastic Rebound Theory• Where the slippage occurs is known as the focus of the earthquake.• The point on the earth surface where the slippage occurs is known as the epicenter.• Seismic Waves are sent outward in all directions from the focus.
    6. 6. Depths of Earthquake Focuses90% of earthquakes have a shallow focus.• Shallow-focus earthquakes have a depth of 70km or less.• Intermediate-focus earthquakes occur at 70-300km.• Deep-focus earthquakes occur at 300-650km.
    7. 7. Major Earthquake Zones• Most earthquakes occur along the edges of lithospheric plates. – The largest zone is known as the Pacific Ridge of Fire. – Second major earthquake zone is along the Mid-Atlantic Ridge. – The third zone is the Eurasian- Melanesian Mountain Belt
    8. 8. Major Earthquake ZonesPacific Ring Mid-ocean of Fire Ridge Eurasian- Melanesian Mountain Belt
    9. 9. Fault Zones• Fault Zones are groups of interconnecting faults that come together on a boundary. – Example: San Andres Fault Zone• Any such movement along the zone could cause a major earthquake.• However, not all earthquakes occur along a plate boundaries.
    10. 10. San Andres Fault
    11. 11. Review Questions1. Explain the rebound theory.2. In earthquakes that cause the greatest damage, at what depth would slippage most likely occur?3. Why don’t earthquakes occur below 650km under the surface?
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