Page 211 - Whole Earth Geophysics An Introductory Textbook For Geologists And Geophysicists
P. 211

193   Contour  map  of observed  the  region  of an  earthquake.   with   focus   view).   the   material,   or  landfill.   dis-   with   Seismic   landfill,   of  amount   Measurements   same   the   intensities   three   the   observed   to   prior   hearing   have   sur-   and   back   with   large   3.12).   lasts   or   3   to   etc.   break,   materials   the   col-   will   freeway   flexible

       Earthquakes   Intensities  generally  decrease   the  earthquake   from   this  map  Anomalously  high  intensities  on  northeast  corner  of  the  map  may  be   with  loose  surficial  such  as  sedimentary  deposits   decrease   conditions.   or  sediments   certain   approximately   of   range   on  depends   were   just  rumble   initially   commonly   (S)   shear   ground   the   be   can   (Fig.   generally   7)   up   last   to   dams   those   as   reinforced,   stru




       of   7.6  FIGURE   intensities  in   distance   (epicenter  in   associated   generally   ground   a   magnitude.   a   is   location   effects   the   a   are   which   later   the   waves   destructive   to   6   can   collapse,   vulnerable,   Unless   7.6).   a   likely   buildings   wood
       Characteristics   in   y   t-Filled               intensities   local   to   unconsolidated   magnitude;   one   the   by   yield  should   there   given   where   hearing  report   earthquake.  They   waves,   (P)   than   amplitude,  shearing   Likewise,  surface   be   can   that   (magnitude   earthquakes   8)   and   especially   (Fig.   more   the   concrete   heavy   light-weight




                   Intensi  PS Localize:   e   Sedimen   Valley   that   so   due  occur   is   there   only   is   expressed   world   the   however,   a   at  observed   about  specific   often   an   during   compressional   motion  ground   large   be   damage.   motion   earthquakes   (magnitude   shear   to  bridges   are   intensity   high   material,   example,   while





                   Si                                    source,  earthquake   Exceptions   where   areas   in   intensity.   there  earthquake,   earthquake,   the   by   around  stations   earthquake,   same   intensity   be   must   one   intensities.   People  Earthquakes   ground   the   the   of   severe   less   and   can  S-waves   The   more   (Rayleigh)   rolling   moderate   in   large   but   and  buildings   sediment  landfill,  or   localizing  waves,   building   the
                                                         the   from  distance   focus.   the   from   tance   amplified   are  waves   the  increasing  locally   given   a   For   released   was  energy   seismic  different   at   the   For  magnitude.   7.6).  The   (Fig.  observed   above;   listed   factors   discussing   when   of  Effects   of  shaking  violent   the   effects   the  feeling   and   amplitudes  smaller   7.7).   (Fig.   waves   face   3.8),  causing   (Fig.   fo





















                                                              =   ea
         5  S,







            Systems,   permission   Detected   awak-   are   windows   build-   ordinary   overturned.   shift   broken.   struc-   landslides   fis-  Broad   Objects


            Dynamic   by   buildings.   slightly.   night,  some   and   outdoors.   run   in  negligible   in   is   Buildings   are   pipes   masonry   Considerable   bent.   surface.


            Earth’s   Reprinted   conditions.   of  floors   rock   may   dishes  Some   and   is   structures,  considerable   furniture   structures.   Underground   Most   are   Rails   ground   different   B.  J.   permission


            From   1995.   Effects   special   upper   outdoors.  At   frightened   falls.   plaster   Damage   Heavy   destroyed.   cracked.   standing,   the   on   Dynamic Earth:  An   by   ed.   with   York.   Maximum   Intensity   XII   XI   X   -IX   VII   VI-VII   Vv   IV   III   II   -   I

            intensity,      Christiansen,  ©   River,  NJ.  :   Observed   under  people,   those   on   automobiles   few   a   rattle.   awakened.   are   overturned.   become   moved.  Some   outside.   run   designed   structures.   designed   collapse.   are   badly   is   remain   seen   are       expected  for   The   Geology,   3rd   Used   1995.   New



       Seismology   of earthquake   H.   E.   few   very   people,  especially   swing.   may   Standing  indoors.   indoors,   by   doors   and   Many  everyone.   are  objects   people   Many   is   and  alarm   construction.   specially   built  poorly   specially   in   partly   and   structures  wooden   ground   structures   ground.   destruction.  Waves   air.   intensity  Highest   From   Physical   Porter,   ©   C.   Sons,  Inc.,   and   Earthquake   Range   =8   74-79   7.0



       Earthquake   Mercalli   Scale   Hamblin   and   Inc.,  Upper  Saddle   by  except   instruments.   by   few   a   objects   noticeably   people   many   Dishes,  windows,   nearly   Unstable  broken.   everyone.   furniture  heavy   in   are  people   of  good   slight   is   in   in  buildings,  great   considerable   is   foundations   their   built   well   destroyed.  The   are   steep   on   slopes.   masonry   any,   appear   the   in   total   the   in  thrown   7.3  TA





       Chapter7   7.2   K.   by  W.   ed.   Prentice-Hall,   Intensity   Not   felt   mostly   by   Felt   Suspended   Felt   by   Felt   ened.   by   Felt   are   by   Felt   Some   Most   ings   Damage   Damage   from   Some   tures   occur   if   Few,   sures   _- Virtually   are



       192   TABLE   7th   of   I   II   Ill   IV   Vv   VI   VII   VIII   IX   Xx   XI   XII
   206   207   208   209   210   211   212   213   214   215   216