Page 204 - 1915, Springs of CA.
P. 204

188                 SPBINGS  OP  CALIFORNIA.
            .  The  analyses  indicate  that the  spring waters  are  secondary- alka-
           line in character with very high tertiary alkalinity and a notable degree
           of primary alkalinity.  The fact  that sulphate  and chlorine radicles
           are  not included  and  that silica  is  reported  as  only  a  trace  renders
           these  analyses  of  doubtful  reliability.
             Like other springs yielding notably thermal carbonated water Carls-
           bad Springs  are marked on Plate III (in pocket).  The slopes  at the
           springs  are  covered  with  lava  that  is  probably  andesite.  For  a
           short distance along the road grade,  1  or 2 miles southward and a'few
           hundred feet higher, however, fine-bedded sediments that are similar
           to the  lake  beds  near  Kelseyville  are  exposed.  At  other  places  in
           this  portion  of  the  county  the  lava  also  appears to  be  present  as a
           thin layer overlying sedimentary material.

                              ASTOBG  SPRING  (LAKE  45).
             A  number  of  years  ago  a  short  prospect  tunnel was  run into  the
           hillside  three-quarters  of  a  mile south of east from Glenbrook post
           office,  which  is  30  miles  north  of  Calistoga.  After  the  tunnel had
           been abandoned as a mining enterprise, the character of the water in
           it was noticed,  and for a short time  the water was shipped in tanks
           to San Francisco,  carbonated,  and bottled  as  a  table  water.  When
           seen in  1910,  however,  the  property was  deserted.  A  reservoir had
           been  formed  in  the  tunnel  by  an  earth  and  board  dam  across  it.
           Although slightly  carbonated, the overflow,  perhaps  one-eighth gal-
           lon  a  minute,  seemed  to  be  mainly of  surface  origin,  and  the  rela-
           tively  small  mineral  content  of  the spring  water,  as  shown by  the
           following  analysis,  tends  to  confirm the  belief  that  it  is  essentially
           a surface  water.  The  analysis, which  is  not complete  and does not
           appear  to  be  very  reliable,  indicates  a  secondary  alkaline  and
           primary saline  water.
                      Analysis of water from Astorg Spring,  Lake  County,  Cat.
           [Analyst, M.  E.  Diebod.  Authority, Register of  Mines, California Min. Bur.  Constituents are in parts
                                       per million.]
                                                                 10' C. (50° F.)
           Properties of reaction:  .
             Primary salinity  ,                     ...._..___.         32
                                                                         17
                                                                         0
             Primary alkalinity   -                                      0
                                                                         51
                                                                         49
                                Constituents.                   By   Reacting
                                                              weight.  values.
           fiodhira (Na).. .......................................................................  16'   0.4$
                                                                 9  9
                                                                        .41
                                                                 18     .92
                                                                 11     .8»
                                                                 3.4    .12
                                                                 3.4    .13
                                                                 62     1.30
           Carbonate (CO3) ........-...........'..............................................  48   1.60
           Silica (SiO?) ........................................................................  32  1.05
                                                                203.7
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