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Case Study 4




                     The Cascades




                     Connecting Canada and the United States









                     Malcolm Cooper                             Geophysical aspects and

                     Introduction                               history of activity
                                                                The  Cascades  form  part  of  the  Pacific  Rim
                     The  Cascades  are  a  700+km  long  group  of   volcanic zone and result from the Pacific Plate and
                     volcanoes as well as non-volcanic origin mountains   its  smaller  companion  the  Juan  de  Fuca  Plate
                     that stretch along the west coast of North America,   being subducted under the North American Plate
                     from  Northern  California,  USA  into  British   (Hill,  2004,  pp4–7). This  960km  long  area  lies
                     Columbia,  Canada  (Hill,  2004;  Dzurisin  et  al,   between 96 and 240km offshore, but produces its
                     2008; Figure CS4.1). At its southern end the range   tectonic effects in the Cascade range. These effects
                     is  about  50  to  80km  wide  and  1370  to  1520m   are  eruptions  and  earthquakes,  all  of  which  are
                     high.  At  its  northern  end  at  Lytton  Mountain   extreme  events.  Most  of  the  major  peaks  are
                     (2049m)  in  Canada,  near  the  confluence  of  the   stratovolcanoes made up of layers of lava and other
                     Fraser  and Thompson  Rivers,  the  range  is  only   volcanic debris, and many are quite young (e.g. Mt
                     16km wide. The tallest volcanoes of the Cascades   St Helens), although some such as Mt Rainier are
                     are known as the High Cascades and include the   thought to be considerably older. However, almost
                     4392m  high  Mt  Rainier.  Overall  the  North   all  the  major  volcanoes  shown  in  Figure  CS4.1
                     Cascades  and  south-western  Canadian  Cascades   have erupted in the past 4000 years, with 7 being
                     are  extremely  rugged,  with  many  of  the  lesser   active  within  the  past  250  years  (Dzurisin  et  al,
                     peaks steep and glaciated, but the majority of the   2008). All are presently classed as active and can be
                     volcanoes lie in Washington, Oregon and northern   expected to erupt in the future.
                     California.                                   This history of activity is also reflected in local
                        In addition to their latent and active volcanism   myth and legend, as is common with geothermal
                     the Cascades are a watershed range that has played   areas (Cooper-Erfurt and Cooper, 2009). Indigenous
                     a  key  role  in  human  settlement  in  the  Pacific   peoples  have  inhabited  the  area  for  thousands  of
                     Northwest of the USA and Canada. Heavy rainfall   years and developed their own beliefs concerning
                     and forest environments produced rivers and lakes   the origin and nature of the Cascades (Cashman
                     as well as good agricultural land and timber for   and  Cronin,  2008). According  to  some  of  these
                     industry. As a consequence the mountains support   tales  the  mountains  Baker,  Jefferson  and  Shasta
                     numerous population centres and are heavily used   were  used  as  refuges  from  a  great  flood.  Other
                     for recreation.
                                                                stories,  such  as  the  Bridge  of  the  Gods  tale,  had










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