Page 265 - 1915, Springs of CA.
P. 265

CARBONATED  SPRINGS.                  245
    moderate amount of solids in solution, being essentially primary  and
    secondary alkaline in character:
      Analysis  of water from  carbonated spring near  North  Fork  of Kern  River,  Tulare
                               County, Cal.
      [Analyst, Oscar Loew (1876).  Authority, Wheeler report.  Constituents are in parts per million.]
                                                           11°  0. (52° F.)
    Properties of reaction:
                                                                  10
                                                                   0
                                                                   0
                                                                  50
                                                                  40
                                                                  32
                                                         By   Reacting
                         Constituents.
                                                        weight.  values.
    Sodium (Na).......................................................................  109  4.76
    Calcium (Ca). .......................................................................  64  3.20
    Iron(Fe)...........................................................................  4.5  .16
    Sulphate (SO*) .....................................................................  Trace.
    Chloride (Cl)... .....................................................................  28  .80
    Carbonate (CO3) -...--.-......-..----......--.... ...................................  220  7.32
    Silica (SiO2)...... ..................................................................  73  2.42
                                                         498.5
                                                             ..........

      The rock of  the valley sides is mainly granitic, the spring probably
    rising from the granitic bedrock that underlies the stream gravel and
    meadow alluvium.  A mile northeastward, along Golden Trout Creek,
    are  cliffs  of  lava,  and  2-J  miles  in  a  direct  line  northeastward,  at
    Natural Bridge,  there is  a large deposit of lime carbonate which has
    been referred to  in the description of Jordan Hot Springs  (Tulare 7,
    p.  53).  It may be that the carbonated water of the present isolated
    spring  in  the  valley  bears  some  relation  to  the  former  carbonated
    springs  at Natural Bridge,  1,600  feet higher,  but the relation is  not
    apparent.  A  fault  that is  considered  to  extend  along  this  part of
    the course of Kern River may,  however,  have determined  the point
    at which the carbonated water now issues.

     CARBONATED  SPRING  IN  TIPPER  PTJNSTON  MEADOW  (TTTLARE  1).
      In  Upper  Funston  Meadow,  about  13  miles  by  trail  northward
    from Kern Lake,  on a plateau  lying  between  two  branches  of Kern
    River,  a  small  spring  furnishes  cool,  moderately carbonated  water,
    and  seems  to  be similar  in  character to  the  one  near  Kern  Lake.
    It is known to campers and cattlemen in the region.
       CARBONATED  SPRING  NEAR  QTJINN  HORSECAMP  (TTTLARE  2).
      Quinn  Horsecamp  is  about  9  miles  in  a  direct line  west  of  Kern
    Lake  but  16  miles  by  trail  over  Coyote  Pass.  Near  Soda  Creek,
    which heads  near  the camp,  there is  a  carbonated spring  of  consid-
    erable flow  that is known to  travelers  over the trails in this region.
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