Page 85 - 1915, Springs of CA.
P. 85

HOT  SPRINGS.                      81
      tide  and is  of  little  importance.  Pyritiferous rock  that borders  the
      coast  here  possibly  furnishes  the  sulphur  constituent  of  the  water,
      and  the  oxidation  of  the pyrite may account  for  the  abnormal  tem-
     perature of the spring.
                    SKAGGS  HOT  SPRINGS  (SONOMA  8).
        Along the southwestern bank of a tributary of Warm Spring Creek
     in  northern  Sonoma  County  three  hot  springs  issue  in  a  distance
      of 75 yards.  At this locality is one of the oldest resorts of the State,
      opened  to  the  public  in  1857.  The  region is  composed  of  old  sedi-
     mentary  rocks,  and  the  springs  rise  from  crevices  in  buff-colored
      material that is  probably sandstone,  though  its  appearance  is  tuffa-
      ceous.  Eastward  along  the  road  to  Geyserville,  a  few  schistose
     ledges,  serpentine  belts,  and  a  little  opalized. rock,  all of  which are
     probably of  the Franciscan  formation,  were  noted.  The  sediments
      are  crushed  and  slickensided  at  many  places  and  show  that  the
     rocks  have  been  much  disturbed.  Such  crushing,  which  was  possi-
      bly  accompanied  by  some  faulting,  may  account  for  the  escape
      of hot water at Skaggs Springs and at other places in these disturbed
      sediments.  The water at Skaggs is not perceptibly sulphureted,  but
     it has a distinct oily pdor and taste.

        Analyses of water from \main spring,  Skaggs Hot Springs, Sonoma  County,  Cal.
                          [Constituents are in parts per million.]

                                                  1           2
                                              54° C.  (129° F.).
      Properties of reaction:
                                                       5            4
                                                       0            0
                                                       0            0
                                                      81           84
                                                      14            12
                                                      119           9
                                              By   Reacting   By   Reacting
                     Constituents.
                                             weight.  values.  weight.  values.
                                              879   38.22   898   39.05
      Potassium (K) ..................................  ..............  9.8   .25   3.8   .096
                                              Trace.   Trace.   .19   .028
                                                3.0   .04   2.9   .042
                                              Trace.   Trace.   .25   .006
      Calcium (Ca) ..................................................  26   1.30   15   .75
                                               61    5.03   55    4.51
      Iron (Fe). ......................................  ..............  5.0   .18   .45   .016
                                              Trace.   Trace.   .04   .004
      Sulphate (SO4). .................................  ..............  26   .54   2.4   .050
      Chloride (Cl) ................... j ..............................  60   1.68   63   1.77
      Iodide (I). ......................................  ..............  1.9   .015   Trace.   Trace.
      Carbonate (CO{). ...............................  .............  1,157   38.58   1,146   38.19
      Metaborate(BOs)..... ..........................  ..............  176   4.10   193   4.49
      Silica (SiOg) ....................................  .  151  5.01  120  3.98
                                             2,555.7     2, 500. 03
                                             1,057  48.00
       1.  Analyst and authority, Winslow Anderson, 1888.
       2.  Analyst, E. W. Hilgard.  Authority, U. S.  Geol. Survey Bull. 32.
          35657° WSP 338 15  6
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