Introduction to Seismic Phenomena
    Lecture 6

    Arch 721, Structural Design for Dynamic Loads, University of Virginia
    Copyright © 1996-2006 Kirk Martini. 10-Oct-2007 10:09
    Table of
    Contents

    Quiz 1 Notes

    Today's topics

    • Mechanisms of earthquakes.
      • Plate tectonics.
      • Fault motions and elastic rebound theory.

    • Seismic hazards
      • Fault rupture
      • Ground failure
        • Liquefaction
        • Land slides
      • Ground shaking
      • Tsunamis

    • Measuring earthquakes and their effects
      • Intensity: Modified Mercalli Scale
      • Magnitude: Richter Scale

    • Assessing hazards at a particular site
      • Risk and return period
      • Seismic risk maps


    EERC


    The Causes and Effects of Earthquakes

    Plate Tectonics and Faults


    [Bolt 78, p. 14]

    A model of underground shocks associated with the 1994 Northridge earthquake in Los Angeles (from the Southern California Earthquake Center).


    [SCEC 1996, /animation.html]

    Seismic hazards

    Fault Rupture

    Ground Shaking

    A structure which straddles a fault rupture will almost surely be destroyed, but that probablity is very low.

    The ground shaking induced by fault rupture causes much more widespread damage.

    The nature of shaking at a particular site depends on many factors concerning the nature and distance of the origin of the earthquake and the surrounding geology.


    [Bolt 78, p. 32]

    Waves propogate through the earth's crusts in several forms. P waves and S waves are most prominent.


    [Bolt 78, p. 29]

    Tsunami

    In addition to fault rupture and ground shaking, shaking can also induce tidal waves, called tsunamis. (from the Cornell Theory Center)


    [CTC 1996, /~devine/tsunami.html]

    Liquefaction

    Liquefaction occurs in loosely packed saturated sand when seismic shaking compacts the sand, resulting in increased pressure in the surrounding water. The pressure in the water can rise to the point where it carries all the stress in the soil, so the sand grains carry no net pressure and can flow past one another.

    Landslide

    Seismic shaking can induce landslides in unstable soil.

    Next: Measuring Earthquakes

     

    Arch 721, Structural Design for Dynamic Loads, University of Virginia
    Copyright © 1996-2006 Kirk Martini. 10-Oct-2007 10:09
    Table of
    Contents