Page 297 - 1915, Springs of CA.
P. 297

SULPHUR  SPRINGS.                    277
               HUEE  HUEEO  SPEINGS  (SAN  LUIS  OBISPO  4).
       Two  groups  of  mineralized  springs,  that  are  known  as  the  Huer
     Huero  Springs,  rise  on  the ranch  of  the same  name,  13  to  15  miles
    .southeast of Paso Robles.  The northernmost, which is known as the
     Old Spring, is on the eastern side of the road and about 1| miles south
     of Creston post office.  The water issues in the stream channel at the
     head of a creek, and yields a small flow of cool sulphureted iron water.
     The locality is well shaded by oaks and willows and has been used as a
     summer camp ground for more  than 20  years.  It is  the site of  the
     Keunard  German  settlement,  which  was  started a  number  of  years
     ago.  The New Springs, which are across a drainage divide and about
     2 miles farther south,  are locally known as iron springs, though their
     water is strongly sulphureted.  They rise for a distance of about 100
     yards  along  a  stream  channel  and  yield  about  2  gallons  a  minute.
     Like the Old Spring,  the New Springs are used by campers.  At both
     localities the water issues from the light-colored granitic material that
     forms  a  considerable  portion  of  the  hills  southeast  of  Paso  Robles.

        SULPHITE  SEEING  IN  CAEEIZO  PLAIN  (SAN  LUIS  OBISPO  12).
       A number of small springs in the region between Paso Robles and
     the San Joaquin Valley are sulphureted, but few of them are of par-
     ticular interest, and very few are of greater use than as cattle-watering
     holes.  One  spring  that is in  the  southern  portion  of  Carrizo  Plain
     has  been  developed  to  the  extent  of  piping  its  water  about  a  mile
     northward  to  a  10,000-gallon  iron  tank  which  supplies  two  cattle
     troughs.  It yields about 3  gallons a minute of strongly sulphureted
     water.
       The  hydrogen  sulphide  of  most  of  the  springs  in  this  region  is
     probably  derived  from  sulphide  minerals in  the sediments  of  Ter-
     tiary  age,  which  form  the greater part  of  the  hills  that  border the
     plains.1

        SULPHUR  SPEINGS  ON  BURTON  MOUND  (SANTA  BAEBAEA  6).
       A number of sulphur springs of small flow formerly issued near the
     beach in  Santa Barbara, from  the slight elevation known as Burton
    Mound, on which the Potter Hotel has been built.  Since the construc-
     tion  of  the  hotel,  about  1901,  the  water  of  the  springs  has  been
     pumped to  a small drinking fountain in the hotel office and another
     at the southeastern border of the grounds.  The springs rise in a small
    basin in the basement of the hotel.  Although considerable difficulty

      1 "Bitterwater Spring" is shown on some early maps, about 15 miles northwest of the sulphur spring in
    Carrizo Plain.  In 1910, however, it wasnot found, and information concerning it was unsuccessfully sought.
    It is probably a minor sulphureted spring near the channel of Bitterwater Creek.
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