Page 171 - 1915, Springs of CA.
P. 171

CARBONATED  SPRINGS.                   155

      The conditions that were observed at the springs in California well
    bear  out  the  facts  that  have  been  recorded  of  springs  elsewhere  at
    which  there  are  notable  deposits.  They show  that the  temperature
    of the water and its rate of cooling, the amount of carbon dioxide that
    is  present, and  the  concentration of  the  solution in other constitu-
    ents as well as calcium all  influence  the  deposition of  calcium car-
    bonate.
                      CARBONATED  SPRINGS.
                        NUMBER  AND  LOCATION.
      The  number  of  carbonated  springs popularly  known  as  soda
    springs in California  is  larger  than  the  number of  hot springs,  but
    few of the former class have been improved to greater extent than to
    form drinking springs at summer resorts.  Most of them are of small
    flow,  but they usually furnish good  drinking waters.
      The carbonated springs (see PI.  Ill, in pocket)  are confined mainly
    to the coastal ranges north of San Francisco  Bay and  to  a belt along
    the  Cascade-Sierran  uplift.  The  rocks  of  these  regions  have  been
    briefly  described  (pp.  7-13)  but  are  discussed  in  greater  detail  in
    connection with the description of the springs.

                JACKSONS  NAPA  SODA  SPRINGS  (NAPA  12).
      One  of  the  best  known  and  most  extensively  developed  mineral-
    spring resorts of  the State is  at Jacksons  Napa Soda Springs, on the
    mountain side 650  feet above  Napa Valley.  The principal buildings
    here,  which were  erected during  the eighties,  are made of a volcanic
    tuff  quarried  near  the  springs.  A  bathhouse  and  a  pavilion  are
    frame structures  of more  recent  date.  The property is  open during
    the summer and provides accommodations for about 250  guests.
      In 1892 Anderson 1  mentioned 27 springs at this place,  but in 1910
    only  four  were  improved  and  made  use  of.  Pagoda  Spring,  which
    rises  in  a  hemispherical  basin covered  by  a roof supported  on stone
    pillars,  is  the principal  drinking  spring,  but when visited  its  visible
    overflow was only about one-eighth of a gallon a minute.  The water
    is strongly carbonated and has deeply iron stained its basin.  Lemon
    Spring,  which  is  similar  in  character  to  the  Pagoda  Spring,  issues
    in  a  stone-roofed  basin  at  the side  of  the  driveway,  25  or  30  yards
    below  the Pagoda  Spring.  Two  other springs  rise  in  a  stone  house
    and  are  covered  by  tanks  that  collect  the  carbon  dioxide  that  is
    given  off.  This  gas  is  used  to  more  heavily  carbonate  the  water,
    which is  piped to  a large bottling house near by.  The water has not
    been  extensively  marketed  east  of  the  Pacific  coast  States,  but  has
    been shipped  to  Asiatic ports.
           i Anderson, Winslow, Mineral springs and health resorts of California, p. 202,1892.
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