Page 52 - 1915, Springs of CA.
P. 52

50                  SPRINGS  OF  CALIFORNIA.

            Analysis of water from House Spring,  California Hot Springs,  Tulare  County,  Cat.
              [Analyst and authority, Curtis and Tompkins (1911).  Constituents are in parts per million.]
          Temperature........................................................................   51° C. (124° F.).
          Properties of reaction:
            Primary salinity................................................................   27
            Secondary salinity..............................................................   0
            Tertiary salinity................................................................   0
             Primary alkalinity... v-.........................................................   68
            Secondary alkalinity............................................................   5
            Tertiary alkalinity.............................................................   63
                               Constituent                     E?   Reacting
                               (,onstituems.                  weight,   values.
          Sodium (Na)........................................................................   60   2.61
          Potassium (K)......................................................................   .92   .02
          Lithium (Li)........................................................................   .36   .05
          Ammonium (Nik)..................................................................   .005   .00
          Barium (Ba) and strontium (Sr)....................................................   0   .00
          Calcium (Ca).......................................................................   1.7   .08
          Magnesium (Mg)....................................................................   .19   .02
          Iron (Fe)........................................................................... \   77   -,
          Aluminum(Al)... .................................................................. f   * 77    " *
          Manganese (Mn)....................................................................   0   .00
          Sulphate (SO4)..-..................................................................   5.5   .12
          Nitrate (NOs).......................................................................   .51   .00
          Chloride (Cl)........................................................................   27   .75
          Bromide (Br) and iodide (I)........................................................  Trace.   Trace.
          Carbonate (COs)................................................................-....   55   1.82
          Metaborate(BOj)...................................................................   S.6   .08
          Arsenate (As04)....................................................................   1.7   .04
          Phosphate (POO....................................................................  Trace.   Trace.
          Silica (SiO2)........................................................................   54   1.78
                                                              	211.055 ..........
          Carbon dioxide (CO2)...............................................................   0   .00
          Hydrogen sulphide (HjS)...........................................................   0   .00
            The analytical data show that the water is soft,  only slightly min-
          eralized,  and  primary alkaline  in  character.  Tertiary alkalinity and
          primary salinity are noteworthy properties.  The proportion of arsen-
          ate radicle is an unusual  feature and should be taken into account in
          using this water.

                      HOT  SPRINGS  NEAR  KERNVILLE  (KERN  11).
            The hot  waters  that rise  at a  number of  places  along  Kern River
          suggest that the lower course of the river, as well as its upper portion,
          which is so mapped  (see  PI. Ill, in pocket), may follow a fault zone.
            About  2  miles  northeast  of  Kernville,  at  the  base  of  steep  slopes
          on  the  eastern  side  of  the  river  valley,  warm  water  seeps  out  at
          several  places,  but  the  main  point  of  issuance  is  in  a  small  marshy
          area in  an  open cove  on  the  valley  side.  A  small  frame bathhouse
          has been  erected  here and  is  used  locally.  The temperature of  the
          water is about 103°, its flow is small,  and it does not taste distinctly
          mineralized.  The  rock at  this  locality  is  a  coarse-textured  granitic
          gneiss  whose  planes  of  schistosity  dip  steeply  eastward  and  strike
          parallel with the valley side.
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