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10.1).   tem-   heat   materials   the   to   upwelling   a     211

                                                      (Fig.   original   of   clues   lithosphere),   floor  away  from
                                                      Earth   the   transfer   Earth   provide   intrusions;   rate

                                                      the   of   the   different   (subducting   ocean   flows  outward,  interior  across  its  cold   surface  ina   average   HFU.
                                                      of  surface   function   a   is   Earth,   the   within   of  ability   rates   flow   igneous  (young   Earth   of  the   “N   Heat   Heat flow  refers  to  the  amount   crosses  the  amount  of  time. The  0.08  W/m’.  equivalent  to   107~*  cal/cem?/s,  or   1.9

                                      temperate),  the
                                            as





                 0              within  a  material.  flowan],  10  move  gently  and  smoothly;  to  pour  out.   the  Earth  across   \emperatus,  gaia.  gt,  the  Earth).  pertaining  to  the  Earth.   with  heat.  L.  gradi,  to  step).  the  amount  of slope,   the  rate  of change   n.,   dé  ant)   within  the  Earth,   the  through  interior   surface  of  the  region   of   heat   the   and  Earth,   heat   of  Measurements   depths   the   into  protruding   (subsidence   t
                 R47          [|OE.  hatu),  the  quality  of being  hot;  energy  manifest  by   <   L.   |<  degree  of hotness;  the  amount  of heat  per  unit  mass  of a  matcrial.   adj.,  having  to  do   thar'm'l  gra’   the   from   a  across   production   the   the   of  regions   10.2).   shallow   at   material   through




                 Poe    Flow    the  accelerated  vibration  of molecules   vi.,  |OE.  heat flow  (het  fld)  n.,  the  rate  of transfer  of heat from   (tem'  prachar)  n.,   <  5).  (Gr.  ged-   n.,  (gra'dé  ant)   |<  of a  road:  the  rate  of change  of a  parameter.   (je'  6  in  temperature  with  increasing  depth   outward   flow   heat   Earth,   the   different   (Fig.   heat   material   hot   of   cold   cooling  of  material   ridge).




                 A            heat  (het)  n.,   (fld)   its  surface.   temperature   (je'   thermal  (thar'm'l)   gradient   geothermal  gradient   flows   Heat   of   rate   The   of  perature   between   conduct   presence   asthenosphere),   the   and   mid-ocean
                 CH     Heat     Slow    geo-                 to









                                                                                                                 i







                                                         Earth's   NJ:   Cliffs,   E.   W.   mag-   and   to   Blackwell   Earth's   pp.   and   Monograph   Magnetic   ridge.   tecton-   and   Geophysical   A.   D.   Cambridge:   anom-

                                                         1995.   Herron.   Marine   reversals.   continents,  Journal   Introduction   The   1983,   Press.  401   Gravity   Geophysicists,  Tulsa:   1966.   earthquake   and  Sheriff.   1963,  Magnetic   199,  pp.  947-949.

                                                         Christiansen.   Englewood   M.   E.   1968.  Pichon.   field   and   An   1984.   Boston:   McElhinny,   Elementary   and   Geophysicists.   Heirtzler.   Pacific-Antarctic   Hotspot:  Contemporary   from   of  Journal   E.   R.   -  Geophysics.


                                                         H.   ed.).   (7th   Dickson,   Le   geomagnetic   floor  of Geophysical  Research.  v.73.  pp.  2119-2136.   Brooks,   Exploration,   Field,  London:  Academic   R.   J.   the  Smith.  R.  B.,  R.T.  Shuey. Jr.,  R.  Pelton,  and  J.  P.  Bailey.   properties   Geldart.   UniversityPress.  860  pp.   ridges.  Nature.  v.
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