Page 122 - 1915, Springs of CA.
P. 122

114                 SPRINGS  OF  CALIFORNIA.

           tively  high  proportion  of  silica  in  the  first  two  is  noteworthy.  It
           is not unlikely that the third also is characterized by a high proportion
           of silica,  and  that  a  typographical error in  the  analytical statement
           is responsible for its  apparently low silica content.
                         FETTERS  HOT  SPRINGS  (SONOMA  19).
             During the summer of  1909  a  bathing establishment which is sup-
           plied  by  four  drilled  wells  was  erected  about  200  yards  east  of  the
           Agua  Caliente  baths.  A  hotel  was  opened  on  the grounds and  the
           place  was  advertised in  1910  as  Eleda  Hot  Springs,  but  it has since
           become known as Fetters Hot Springs  (PL  VII,  O,  p.  108).
             The hills that border the eastern side of Sonoma Valley are of rhyo-
           litic lava, and the wells at the several resorts are drilled into volcanic
           tuff that underlies the thin layer of alluvium in this part of the valley.
           The presence of the lava, which is thought to be of a relatively recent
           geologic  period  of  effusion,  suggests  that a  rather high  temperature
           gradient  accounts  for  the  thermal  character  of  the waters  and that
           the  structure  probably furnishes  the  artesian  conditions.
              WARM  SPRINGS  OF  STATE  HOME  AT  ELDRIDGE  (SONOMA  16).
             Warm  springs  that  seem  to  be  similar  in  origin  to  the  artesian
           waters  of  the  resorts just  described  issue  at  several points  north of
           Sonoma Valley.  At the vegetable and dairy farm of the State Home
           at  Eldridge water  72° in temperature is obtained from a spring that
           yields  about  10  gallons a minute of  water that is used  in  the dairy
           and for irrigation.  The water broke forth at this spring at the time
           of the earth'quake of April 18,  1906, and a flowing well 50 yards north-
           ward ceased to flow.  A light-colored tuffaceous rock is exposed a few
           yards from the spring.

                      LOS  GUILICOS  WARM  SPRINGS  (SONOMA  15).
             On  the banks of Sonoma Creek,  about  1£ miles southwest of Ken-
           wood are two springs which yield, respectively, about 2  and 3  gallons
           a  minute  of  water  at  temperatures of  78° and  82°.  In 1909  there
           was a small bathing pool and an old hall or pavilion at the spring near
           the  eastern  bank  of  the  creek;  at  the  other spring,  on  the  opposite
           bank,  there  was  a  small  pool  inclosed  by  an  old  bathhouse.  The
           place  was  used  as  a  camping  resort,  and  several  cottages  had  been
           erected among the trees near by.

                   WARM  SPRINGS  ON  McEWAN  RANCH  (SONOMA  14).
             Large warm springs that are probably similar in origin to the Los
           Guilicos springs and others farther south, issue on the McEwan ranch,
           about  1J miles  west of Los Guilicos Warm Springs.  A part of their
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