Page 138 - 1915, Springs of CA.
P. 138

128                 SPRINGS  OF  CALIFORNIA.
                           HIGHROCK  SPRING  (LASSEN  19).
             A large thermal spring rises on the Highrock ranch,  about 10 miles
           south  of  east from  Amedee.  Its water is  used  for  domestic  supply
           and for irrigation,  and  the spring forms  a convenient watering place
           on  the road  between. Honey Lake Valley and  Reno,  Nev.  Measure-
           ments in  1909  showed its flow to be about 525 gallons a  minute and
           its temperature 860.1  The water does not have a distinctive alkaline
           taste, but it is said to rust tinned-iron vessels quickly.
             The  spring rises  at  the  edge  of  Honey Lake  Valley,  from  basaltic
           lava  that forms  the hills  to  the  east.  No  deposit  of  note is  observ-
           able  immediately  at  the  spring,  but  30  yards  northwestward  are
           prominent calcareous tufa crags from which the ranch takes its name.
           The  deposit  covers  an  area  of  perhaps  2  or  3  acres,  and  its  well-
           developed crags are coated with dendritic tufa.  Water does not now
           issue from the tufa,  but there is said to be an Indian legend  that the
           main spring formerly did so.

                            KRUGER  SPRING  (PLUMAS  11).
             At  the upper end  of Indian Valley in  Plumas  County, in meadow-
           land a mile east of Greenville, there is a thermal spring that has been
           known  as  Kruger  Spring  since  the  late  eighties.  During  the  more
           prosperous days of mining in this region it was extensively patronized
           as  a  bathing place.  Of late years,  however,  the  bathhouse has not
           been kept in repair and it has not been open to  the public.  In 1909
           about  1  gallon  a  minute  of water  94°  in  temperature flowed  from,  a
          board-curbed pool in the bathhouse.  Both the temperature and  the
          yield  could  probably  be  increased  by  sinking  a  well  casing  into
           the spring.  A few bubbles of gas rise in the pool,  but the water has
          no  distinctive  taste or  odor.  The  spring may furnish  evidence  that
           there has been faulting through Indian Valley;  It seems more prob-
           able,  however,  that  alluvial  artesian  water  is  here  brought  to  the
          surface,  possibly by a buried ridge.

                          MARBLE  HOT  WELLS  (PLUMAS  16).
             In Sierra Valley, in the southeastern part of Plumas County, several
          flowing artesian wells discharge water of unusually high temperature.
          The most remarkable of these wells are on the Marble ranch, at Kettle
          post office,  where,  in  1885  and  1888,  two  wells,  4  inches in diameter,
          were  sunk  about  100  yards  apart  to  a  depth  of  350  feet.  Each  of
          these wells discharges about  175  gallons  a minute  of  scalding water,
          the  recorded  temperatures  being  156°  and  161°.  A  third  well,  150
          yards west of the other two, was sunk to a depth of 450 feet, at which
            i In 1882 Russell reported its temperature to be 100° (U. S. Geol. Survey Mon. 11, p. 52), but it is doubtful
          whether such a marked reduction  in temperature has really taken place.
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