Page 42 - 1915, Springs of CA.
P. 42

40                   SPRINGS  OF  CALIFORNIA.

             The  ravine  in  which  these  springs  issue  is  steep,  with  narrow,
          precipitous  sides,  and  the  rock  exposed  is  largely  a  crushed  gneiss.
           Recent landslide patches within it also indicate the broken and dis-
           turbed  character  of  this  area  and  furnish  local  evidence  that  the
           thermal character of the springs is due to crushing and slipping of the
          rocks.
                         PILARES  HOT  SPRING  (RIVERSIDE  7).
             In the channel of San Jacinto Kiver, about 6 miles west of the base
          of  the  San  Jacinto  Range, warm water  rises  and  forms  a  tule  area
          several  acres  in  extent.  The  water  was  formerly  piped  to  a  bath-
          house on the higher land, but in  1910  a  hut  among the  tules  formed
           the  local  bathing place.  Though  the  abnormal  temperature of  this
          water may be due in part to leakage of deep-seated hot water upward
           through  the  San  Jacinto  fault into  the alluvium  of  the  valley,  it is
          more probable that a buried spur of a granitic ridge that here borders
           the valley acts as a dam and forces alluvial water to the surface from
           a  depth sufficient  to  account for its  temperature.  A  well  that was
           drilled a couple of hundred yards west of the spring obtained a warm
           artesian flow.
                            PALM  SPRINGS  (RIVERSIDE  11).
             At Palm Springs,  at the southern base of San Jacinto Peak,  a rise
          of  thermal  water  tends  to  confirm  the  topographic  evidence  that
          faulting  has  taken  place  in  this  vicinity.  The  water,  which  has  a
           temperature of about  100°,  is  used for bathing,  and  there is  a small
          health  resort  here  on  the  edge  of  the  desert.  These  are  the  same
          springs  that were  formerly known  as  Aguas  Calientes  (hot  waters),
           and the following partial analysis of the water was early made:

                    Analysis of water from Palm Springs, Riverside  County,  Cal.
                [Analyst, Oscar Loew.  Wheeler report (1876).  Constituents are in parts per million.)
                                                                 38° C. (100° F.)
           Properties of reaction:
                                                                        77
                                                                         0
                                                                         0
                                                                        23
                                                                      Trace.
                                                                         ?
                                                               By   Reacting
                                Constituents.
                                                              weight.  values.
                                                                 158   6.87
           Lithium (Li)...... .................................................................  Trace.   Trace.
                                                               Trace.   Trace.
                                                               Trace.   Trace.
           Sulphate (SOi)... ....... ............................................................  Trace.   Trace.
          Chloride (Cl)... ................... ..................................................  188   5.30
                                                                  47   1.57
          Silica (SiOi). .......................................................................  Trace.  Trace.
                                                                 393
                                                               Trace.  Trace.
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