Page 367 - 1915, Springs of CA.
P. 367

MINOR  PERENNIAL  SPRINGS.               347
    tule-grown  stream,  that  has  a  flow  of  about  3  gallons  a  minute
    near the road.  It supplies a watering trough and has also been used
    for garden irrigation.

               CACTUS  FLAT  SPRING  (SAN  BERNARDINO  30).
      Cactus  Flat Spring,  which is  also  known  as  Hidden  Spring,  issues
    from an adit excavated in the hard, granitic material in the side of a
    ravine.  The water is collected in a small reservoir formed by a dam,
    across  the  ravine,  and  has  been  used  for  more  than  20  years  for
    domestic supply and for irrigation.  It furnishes a convenient water-
    ing place on the stage road from Victorville  to Bear Valley.

                SARAGOSSA  SPRING  (SAN  BERNARDINO  31).
      Saragossa Spring is about 2 miles in a direct line or 3 miles  by road
    southwest  of  Cactus  Flat  Spring.  It  has  been  developed  by  an
    excavation  in  gray  granitic  material  and  yields  a  small  domestic
    supply  that is  of  value in  this  poorly watered  portion  of  the  moun-
    tains.
              MONTE  CRISTO  SPRING  (SAN  BERNARDINO  32).
      Monte Cristo Spring  is  in Van Dusen Canyon,  a  mile  or more in a
    direct  line  southward  over  Gold  Mountain  from  Saragossa  Spring.
    It yields  about  1  gallon  a  minute  of  cool,  fresh water  that supplies
    the camp  of  the Rex Mining Co.,  which has been  driving the Monte
    Cristo tunnel into the mountain.

            WARRENS  RANCH  SPRINGS  (SAN  BERNARDINO  39).
      Warrens  Ranch  Springs  are  situated  a number  of  miles  southeast
    of  Cactus  Flat,  in  a  pass  on  the  opposite  slope  of  the  mountains.
    The  ranch is  28  miles  eastward from Banning,  on  the  main road  to
    Dale mining camp,  and is  a regular stopping place for travelers.  Its
    water is obtained from large springs below  the ranch  and is pumped
    to it by a gasoline engine.
      The springs at the six localities last described  (San Bernardino 28,
    29,  30,  31,  32,  and  39)  are  among  those  principally  used  of  the
    numerous  springs  that  rise  in  San  Bernardino  Mountains.  All  of
    them  are  of  surface  origin  and  owe  their permanence  to  the precipi-
    tation on  the slopes  of  the mountain range,  whose higher peaks  are
    capped with snow during a part of the year.

                   PALMDALE  SPRINGS  (RIVERSIDE  12).
      An  agricultural settlement was started at Palmdale,  8  miles south
    of Palm, Springs railroad station,  a number of years ago, but in 1909
    the place was nearly abandoned.  Water for irrigation was furnished
    partly by a group of springs that yield a considerable supply.
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