Page 148 - 1915, Springs of CA.
P. 148

136                 SPRINGS  OF  CALIFORNIA.
          line that, if extended southeastward, would pass 8 miles north of the
          Mono Basin Warm Springs  (Mono 8,  p.  145).
                          BENTON  HOT  SPBING  (MONO  12).
            About 300 yards northwest of  the store and post office at Ben ton, at
          the base of slopes  that border an area of meadowland, is a spring that
          forms a shallow pool approximately 10 feet in diameter in which  the
          water has an observed temperature of 135°.1  It has furnished a sup-
          ply of water for  the  town for  domestic  and irrigation uses  since  the
          sixties, and in the early days it also furnished power for a small stamp
          mill.  Its  discharge  is  approximately  400  gallons  a  minute.  The
          water as it rises effervesces with a gas that is probably carbon dioxide.
          A small amount of an efflorescent salt probably Epsom salt forms
          near  the  margin  of  the  pool.  A  quantitative  analysis  of  the  water
          is not at hand, but the total amount of solids in solution has been given
          as  260  parts per million.2
            The surrounding region is mainly granitic,  but the slopes immedi-
          ately north of  the springs  are of white volcanic  ash or tuff that con-
          tains  rounded  lava  gravel.  This  material  lies  nearly  horizontal  on
          weathered gray granite.  In a  canyon half a mile west of  the spring
          are numerous bands of dark basaltic material, up  to  2  feet in  thick-
          ness,  that  are,  however,  considered  to  be  inclusions  and  not  intru-
          sions in the granite.  The ultimate association of lava with the gran-
          ite,  both of  the  tuff and  the inclusions,  suggests  that here  again  the
          lava offers an explanation for the existence of the spring and also for
          the quantities of carbon dioxide that rise with  the water.
                     WARM  SPBING  IN  SALINE  VALLEY  (INYO  12).
            There are a few thermal springs of minor importance in the desert
          region of eastern California.  One of these springs is at the northeast
          side of Saline Valley,  about 25 miles in a direct line east of Independ-
          ence.  It yields a small flow,  and its water is not of high temperature.
          There are  several cool springs a short distance westward from it and
          also  to  the  southeast  that form  watering places in  this part  of  the
          desert.
                    WABM  SPBING  IN  PANAMINT  VALLEY  (INYO  29).
            About 4 miles north of Ballarat,  on the eastern edge of Panamint
          Valley, is a spring similar  to  the  one  in  Saline Valley.  Its water is
          tepid  and  is  noticeably sulphureted,  and  its  yield  is  only  about  40
          barrels  a  day  (1  gallon  a minute).  It forms  a small watering place
          on  a road leading northward from Ballarat.
            1  A temperature of 138° was recorded in this spring in 1876 by the Wheeler Survey (U.S. Geog. Surveys
           W. 100th Mer., 1876, p.  196),  where  it is  stated  that  the  temperature  is considered to vary 5°.  In the
           Eighth Report of the California State Mining Bureau, 1888, pp. 356 and 357, temperatures of 135.5° in 1870
          and 134.6° in 1888 are recorded.
            2 Wheeler, G. M., U. S.  Geog. Surveys W. 100th Mer., 1876, p.. 196.
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