Page 175 - 1915, Springs of CA.
P. 175

CARBONATED  SPRINGS.                   159
      The  analyses  indicate  that  the  waters  are  all  of  the  same  general
    primary alkaline type, but they show minor differences in the relative
    proportions of  calcium and magnesium and of  sodium and  potassium
    and  in  the  content  of  silica,  iron,  and  aluminum.  The  Wenzell
    analyses  alone  report  borates,  but  it  is  not  unlikely  that  tests  for
    borates were not  made  by the  other  analysts  and  that  borates  are
    reported  as  carbonates.  The  great  similarity  of  the  three  analyses
    by  Bauer  and  the  apparent  change  in  composition  of  the  American
    Ems  Spring water are  of interest.
      The  rocks  about Mtna,  Springs  are  the  altered  sediments, opaline
    material,  and  associated serpentine  of  the Franciscan formation.  A
    short  distance  northward,  near  some  of  the  quicksilver  workings,
    lava covers the surface.

                 WALTERS  MINERAL  SPRINGS  (NAPA  3).
      About  10  miles by road east of Minsk  Springs,  on  the eastern side
    of the canyon of Pope Creek,  there are  two small carbonated springs
    that  have  long  been  known  as  Walters  Mineral  Springs.  They
    issue  about  150  yards  apart  and  350  feet  above  the  creek,  on  the
    side  of  a  ravine  in  an  area  of  serpentine.  The  rock  has  decayed
    sufficiently  to  form  a  red  clay  soil,  but  many  bowlders  outcrop  on
    the hillsides.  The water has a distinctly sweet taste, and the analysis
    tabulated  on  page  160  shows  that  it  contains  a  high proportion of
    magnesium, being secondary alkaline in character.
      The  magnesian  character  of  the  water  is  worthy  of  note  in  con-
    nection  with  the  serpentine  at  this  locality.  The association with
    serpentine  (a  magnesium-bearing  rock)  of  mineral  springs  having a
    high  content  of  magnesium would  be  expected, however,  and  it has
    been  already  mentioned  in  the  discussion of the relation of the min-
    eral character of sorings to  the rocks  through which  they rise.  (See
    p.  160.)
      Walters  Mineral  Springs  have  been  improved  as  a  resort  since
    about  1902.  In  1910  there  were  two  new  frame  buildings,  having
    accommodations  for  50  people,  and  a  pavilion  at  the  lower  spring
    that provided a place for dances and  other social gatherings.  Water
    from this spring  has been bottled and marketed to a small extent for
    table use.
                    SAMUEL  SODA  SPRINGS  (NAPA  7).
      About 6  miles southeast of  Walters Mineral Springs,  and  also  well
    above  Pope  Creek but  on  the  other side  of  its  canyon,  Samuel Soda
    Springs  form  another  group  that has  long  been  known.  The  place
    has been improved  as  a  resort for  a  number  of years,  and  the water
    has  also  been  sold  as  a  carbonated  table water.
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