Page 120 - 1915, Springs of CA.
P. 120

112                 SPRINGS  OP  CALIFORNIA.
             The water of the White Sulphur Spring is  characterized chiefly by
           primary salinity and primary alkalinity with high tertiary alkalinity.
           It is  possible  that the latest analysis represents a different water from
           that represented  by the other two  analyses,  though the spring name
           is  the  same  for  all.  If,  however,  the  three  analyses  represent  the
           same  water,  they indicate  that  a  gradual loss  of  carbon  dioxide  and
           hydrogen  sulphide,  accompanied  by  increase  in  concentration,  has
           been taking place.  The net result of these changes has been increase
           in  primary  alkalinity,  decrease  in  secondary  alkalinity,  and  a  very
           great decrease in tertiary alkalinity.
             Though  the analyses  of  the other springs show  differences in con-
           centration  and  in proportion  of  minor  constituents,  their waters  are
           much  alike  in  general properties  of  reaction,  approaching sea  water
           in  character  but  differing  from  it in  containing  a  less  proportion  of
           magnesium and sulphate radicles.  The presence of rare constituents
           in  waters  of  such high  concentration  is  to  be  expected.  The  water
           of  the Black Sulphur Spring appears  to  be a relatively pure solution
           of common salt,  and  the  "Surprise"  is noteworthy for its great con-
           centration more than nine times that of sea water.
             The adjacent hills  are  composed  of  cherty gravels  and  other finer
           sediments that represent marine deposits, but the origin and character
           of the springs seem to be due to the local formation of a saline marsh.
           Several unsuccessful attempts have been made to obtain fresh water
           here,  and  in  1908  the  domestic  supply  was  pumped  from  a  well  If
           miles eastward.
                           BOYES  HOT  SPRINGS  (SONOMA 20).
             A number of small warm springs issue along  Sonoma Creek,  a few
           miles north of  San Pablo  Bay.  Artesian wells  that also  yield  warm
           water have been drilled at several places on the eastern side of Sonoma
           Valley,  and  at  three  places  where  such  wells  have  been  obtained
           resorts have been built up that are well patronized during the summer
           months,  as  they are  only a two  and  a half hours'  ride by train from
           San  Francisco.  Boyes  Hot  Springs,  about  2  miles  northwest  of
           Sonoma, is the southernmost of these resorts.  Here a hotel and sev-
           eral  cottages  and  tent  houses are situated  in  a  grove of  oaks, and a
           quarter  of  a  mile  northwest  of  the  hotel  a  large  swimming  plunge
           and tub baths are supplied by water pumped from two wells.  These
           are  said  to  be  200  feet  deep,  and  the  temperature  of  the  water  is
           reported  to  be  114°  and  118°.  The  wells,  the  first  of  which  was
           drilled about  1890,  flowed until a short time  after the earthquake of
           April 18,  1906,  but the water usually stands a few feet below the sur-
           face.  A third,  unused well 300  or 400  yards to  the east was flowing
           about  3  gallons  a minute  in  December,  1909.  The water is  bottled
           for table use, and an analysis of it is tabulated  (p. 113) for comparison
           with analyses of other similar waters of this valley.
   115   116   117   118   119   120   121   122   123   124   125