Page 65 - 1915, Springs of CA.
P. 65

HOT  SPRINGS.                      61

        The  springs  at  this  place  were  known  to  the  Catholic  mission
      fathers,  who  at  one  time  lived  here.  Their  extensive  modern  use
      dates  back  more  than  20  years,  and  their  accessibility  has  made
      them an objective point for  automobile parties.  In  1908  accommo-
      dations were  provided  in  hotels  and  cottages for  about  200  guests,
      while tub and plunge baths at the Soda and the Sulphur springs, and
      a  swimming  plunge  that  was  also  supplied  by  these  springs,  gave
      ample  opportunity  for  use  of  the  waters.  Analyses  of  the  springs,
      made a number of years ago,  are available and are here presented in
      the standard form.

              Analyses of water from Paraiso Hot Springs,  Monterey  County,  Cal.
                          [Constituents are in parts per million.]
                             1        2        3        4        5

      Temperature. ................ 48°C.(118°F.) 48°C.(118°F.) 46°C.  (114°F.) 21°C.  (70°F.) 21°C. (70°F.)
      Properties of reaction:
                               81       85        69       51        82
         Secondary salinity. ......  2   0        10        0        17
                                0        0         0        0        1
         Primary alkalinity. . .....  0  2         0       11        0
         Secondary alkalinity .....   17   13     21       38        0
         Tertiary alkalinity. ......  22  12      39       28        51
                                   By
                                                      By
                          weight.  R e a  values.  weight.  R e a  ting  values.  By  weight.  R e a  ting  values.  weight.  R e a  ting  values.  weight.  R e a  ting  values.
                          By
                                                               By
                                                                   c
                              c  ting
                                                 c
                                       c
                                                          c
           Constituents.
      Sbdium (Na).. ............... 253   11.00 252   10.96   233  10.13   234  10-18  179   7.78
       Potassium (K)...............  2.9   .07   3.1   .08   6.4   .16   80   2.05   58   1.48
      Calcium (Ca)....... ..........  41   2.04   32  1.60  28   1.40   30   1.50   23   1.15
                          7.5  .62          38   3.13  74  6.09  9.8  .81
      Iron (Fe).. ..................  7.3   .26   }»  .35  .43  3.9  .14
      Aluminum ( Al) ..............  5.1   .56   .68  9.7  12
       Sulphate (SO4).. ............. 493  10.27  463   9.64   520   10.83  23   .48   22  .46
      Chloride (Cl). ....... .........  38   1.07   39   1.10  29   .82   342   9.65  387  10.92
                          79  2.63  56  1.87  94  3.13  304  10.13
       Arsenate ( AsOi) ............. "so"" ~"l"66" "45"" "i.'ig" ""44"" "i."46" Trace. -Trace.  "176"" ""5." 84
      Silica (Si02)  ...............                  156  5.18
                         976.8    909.1    1,002.1   1,255 ....... 858.7 .......
       Carbon dioxide (CO2). .......  25  1.14  (a)  (a)  17  .77   (a)  (0)
                                            60   3.52
                                   a Present.      t
        1.  Hot Soda Spring.  Analyst and authority, Winslow Anderson, 1889.
        2.  Hot Soda Spring.  Analyst, A. Cihi, 1871.  Authority, U. S. Geol. Survey Bull. 32.
        3.  Hot Sulphur Spring.  Analyst and authority, Winslow Anderson, 1889.
        4.  Arsenic Spring.  Analyst, A. Cihi (?).  Authority, advertising matter.
        5.  Iron Spring No. 2.  Analyst, A. Cihi (?).  Authority, advertising matter.
         The Hot Soda Spring is primary saline in character with secondary
       alkalinity  as  a  subdominant  property.  The  name  "Soda,"  given
       to this spring,  is  a misnomer, as the word usually applies to primary
       alkaline waters.  The Hot Sulphur Spring differs from the Hot Soda
       Spring  chiefly  by reason  of  higher  secondary  salinity  and  its  con-
       tent  of  hydrogen  sulphide.  The  analyses  of  the  Arsenic  and  Iron
       springs  are  of  doubtful  authenticity.  It is  of interest  that only  a
       trace  of  arsenic  was found  in the Arsenic Spring  and very little iron
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