Page 39 - 1915, Springs of CA.
P. 39

HOT  SPRINGS.                      37
      rather  than  from  constituents  in  deep-seated  hot  water  that  may
      enter the alluvium.
                    FAIRVIEW  HOT  SPRING  (ORANGE  1).

        A warm spring or well at Fairview Hot Spring, in the coastal plain
     south of Santa Ana,  resembles in occurrence the Harlem and Urbita
     springs.  Originally  the  Fairview  Spring  was  a  natural flow,  but  a
     casing  that  was  sunk  to  a  depth  of  700  feet  into  it has  converted
     it into a flowing  artesian  well.  In  1908  a hotel and  cottages  pro-
      vided  accommodations  for about 50 people.  The water rises with a
      temperature of  96°  and supplies  a swimming plunge  and  tub baths.
     The discharge varies somewhat with the season;  in December,  1908,
     it was  about 15 gallons a minute.  An odorless, inflammable gas rises
     with the water and is  burned for cooking and lighting.  The water,
     which is colored brown, doubtless from organic stain, has been placed
     on  the local  market for table use  under the label "Amberis Water."
     Although  the water has  a faint oily  taste, it is  thought to be essen-
      tially ground water that here rises through the deep  alluvium which
     forms  this  part  of  the  coastal  plain.  Its  origin  is  probably not  re-
     lated to the shales of the oil-bearing series of southern California that
     form  low  hills  a  mile  southward,  except  as  these  shales  act  as  an
     underground dam that forces  the alluvial water of the artesian basin
     of this region to the surface.

                    EDEN  HOT  SPRINGS  (RIVERSIDE  8).
        Along  the western  base  of San Jacinto Mountains  are several  hot
     springs  that  have  already  been  mentioned  in  their  relation  to  the
     San  Jacinto  fault.  At  Eden  Hot  Springs,  the  northernmost  group
     along this  fault,  about eight small springs  rise within  a  distance  of
      100 yards at the base of a steep granitic slope.  The water issues less
     than  200  yards  beyond  the southeastern  border  of  a series  of shales
     and sandstones  of Tertiary age,  in which  there  are  dislocations  that
     were probably caused by the uplift of the San Jacinto Range;  but the
     springs  seem not to be related  causally to the sediments.  The max-
     imum  temperature  of  the  water  is  about  110°.  It  is  moderately
     sulphureted  but does not  seem  to be otherwise notably mineralized.
     During  1909  water from  two  of  the springs  was placed  on  the local
     market  for  table  use  under  the  labels  "Iron  Lithia"  and  "White
     Sulphur."
       A small resort has  been  maintained  at the place for  a  number  of
     years.  In  1908  cottages  and  tents  provided  accommodations  for
     about 50  people,  and  a bathhouse  and small swimming pool allowed
     use of the water for bathing.
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