Page 274 - 1915, Springs of CA.
P. 274

254                 SPEINGS  OF  CALIFOENIA.

                   ST.  HELENA  WHITE  SULPHUR  SPRINGS  (NAPA  10).
             St.  Helena  White  Sulphur  Springs  are  situated  in  the  canyon  of
           Sulphur Creek,  2  miles southwest of  the  town of  St.  Helena.  They
           form  the  nucleus  of  an  old  and  formerly  a  well-known  resort,  but
           about 1904 the hotel was destroyed by fire,  and in 1909 the improve-
           ments  had  not  been  extensively  rebuilt.  There  were,  however,
           cottages  and  an open screened  dining room,  furnishing  accommoda-
           tions  for  about  25  people,  and  a  small  bathhouse  near  one  of  the.
           springs.
              Analyses of water from St.  Helena  White Sulphur Springs,  Napa  County,  Cal.
                               [Constituents are in parts per million.]
                              I         2         &         4        5

                          25° C.  770  T7  \  69°  F.)  32° C.  ( qn°  TT  t  30°C.(S56°  F.)  21°  C.  (70°  F.)
           Properties of reaction:
             Primary salinity..   83       59        82        80        6S
             Secondary  salin-
               ity ..............  4        0         1        5          1
             Tertiary salinity. . .   0     0         0        0          0
             Primary  alkalin-
               if-rr              0         5         0        0          0
             Secondary  alka-
               linity... ........  13      36        17        15        35
             Tertiary alkalinity  21        9        22        13    (?)
                              React-     React-    React-    React-   React-
                          By
                                                         By
                                     By
                                               By
                                                                  By
              Constituents.  weight.  ing   weight.  ing   weight.  ing   weight.  ing   weight.  ing
                              values.    values.   values.   values.  values.
                          218   9.48  136  5.91  207  8.99  232 10.05  177  7.70
                           23   1.15  42  2.10  28  1.40  29  1.45  49  2.45
           Magnesium (Mg) ......  10   .82   15   1.23   6.8  .56  13  1.03  24  2.00
                           2.0  .22  5.6   .62
                          123        83   1.73  96  2.00  131  2.73  149  3.10
           Chloride (Cl)..........  260  7.33  133  3.75  251  7.08  280  7.90  164  4.63
           Sulphide (S) ..........  9.4  .59  TYni>A  a 19  1.20  a 13  a 12  .75
           Carbonate (CO3) ......   29   .97   113  3.76   20  .67  32  1.06  110  3.67
           Silica (SiO2)... ........  11  .36  25  .83
                          685.4     552.6     627.8       730      685
           Hydrogen   sulphide
            (H2S). ..............  34  2.01    41   2.38  28  1.64     Trace.
            a Reported as sodium and calcium sulphides.  Recalculated  on  assumption that 41  per cent is CaS and
           59 per cent Na2S by comparison with analysis of spring No. 5.
            1.  Spring No. 5.  Analyst and authority, Winslow Anderson (1888).
            2.  Spring No. 9.  Analyst and authority, Winslow Anderson (1888).
            3.  Spring No. 2.  Analyst, J. Le Conte (1871).  Authority, U. S.  Geol.  Survey Bull. 32.
            4.  Spring No. 6.  Analyst, J. Le Conte (1871).  Authority, U. S.  Geol. Survey Bull. 32.
            5.  Spring No. 7.  Analyst, J. Le Conte (1871).  Authority, U. S.  Geol. Survey Bull. 32.
             The  group  includes  five  noteworthy  springs which  issue within a
           space of  150 yards near the foot of  the slope 011  the northeast side of
           Sulphur  Creek.  All  these  springs  were  formerly  improved  with
           brick basins, but when visited the northern two were the ones chiefly
           used.  One  of  these formed  a  drinking pool that yielded  about one-
           half  gallon  a  minute  of  mildly  sulphureted  water.  The  northern-
           most  spring,  which  is  about  25  yards  beyond  the  drinking  spring,
           was  surrounded  by  a  cement  reservoir  and  yielded  warm,  mildly
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