Page 302 - 1915, Springs of CA.
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282                 SPRINGS  OF  CALIFORNIA.

                        SANTA  FE  SPRINGS  (LOS  ANGELES  14).
             Three wells that were put  down in the coastal plain 15 miles south-
           east of Los Angeles by Dr. J. E. Fulton, during the seventies, obtained
           sulphur water,  and as the locality was favorable  a hotel was built,  a
           swimming plunge was constructed,  and the property was early made
           a resort, under the name of Santa Fe Springs,  or Fulton Wells.  The
           hotel burned  a  number  of years  ago,  and  the plunge has  been filled
           up,  but when visited in 1908  the place was still conducted in a small
           way as a resort,  there being three small cottages and a bathhouse on
           the  property.  Windmills  over  two  of  the  wells  100  yards  or  more
           from the cottages pumped the water into a tank, whence it was piped
           to a heating boiler and to the baths.  The third  and innermost well,
           which is near the cottages, was equipped with a hand pump.  Water
           from  this  well  was  formerly  bottled  for  table  and  medicinal  use.
           The following  analysis  shows  it to  be  a  secondary  alkaline  and  pri-
           mary  and  secondary  saline  water  that  contains  a  large  proportion
           of iron:

              Analyses of water from east well,  Santa Fe Springs, Los Angeles  County,  Gal.
                               [Constituents are in parts per million.]
                                                       1           55

           Properties of reaction:
                                                           20            24
                                                           30            31
                                                            0            0
                                                            0            0
                                                             50
                                                                         45
                                                         High.        High.
                                                   By   Reacting   By  Reacting
                          Constituents.
                                                  weight.  values.  weight.  values.
           Sodium (Na)...................................................  84  3.63  90  3.89
          Calcium (Ca).. .................................................  205  10.21  167  8.31
           Magnesium (Mg). . .............................................  50  4.08  47  3.86.
           Iron (Fe).. ....................................................  97  3.47  107  3.84
           Sulphate (SO*).................................................  294  6.12  »278  5.78
          Chloride (01)...................................................  100  2.81  108  3.05
          Sulphide (S).... ...:...........................................  6.3  .39
          Carbonate (CO3). ..............................................  374  12.46  320  10.68
          Silica (SiO2).... ................................................  42  1.39
                                                   1,246       1,123.3
          Carbon  dioxide (CO2) ..........................................
               a Reported as "sulphur;"  recalculated from CaSO* by comparison with the other analysis.
            1.  Analyst and authority, Winslow Anderson (1888).
            2.  Analyst, Price and Hewston.  Authority, TJ.  S.  Geol. Survey Bull. 32.
            A number of other wells in this coastal plain area of southern Cal-
          ifornia yield water that is noticeably sulphureted but not so strongly
          mineralized as is.the water of Santa Fe Springs.  Seepages of sulphu-
          reted  water  also  issue  from  shales  at  a  few  places  along  the  coast.
          One  strongly  sulphureted  spring  of  this  character  issues  from  the
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