Page 190 - 1915, Springs of CA.
P. 190

174                 SPRINGS  OF  CALIFORNIA.
            a  collecting  tank  and  a  bathhouse  containing  two  compartments
            have furnished means for bathing.  The water issues from dark shale
            that is here exposed  beside  the creek and deposits considerable lime
            carbonate.  The  two  principal  drinking  springs  are  at  the  camp
            grounds, which are  a quarter of a mile southward up the ravine,  and
            issue  from  seams  in  coarse-textured  sandstone,  one  of  them  at  the
            creek  edge,  the  other  about  25  yards  farther  upstream  and  3  or  4
            yards from the creek.  Both are carbonated and deposit considerable
            iron.  On the slopes within 100 yards of these springs there is a small
            area  of  mica  schist  and  pyroxene  rock  associated  with  outcrops, of
            cherty  material,  which  is  worthy  of  note  in  connection  with  the
            deposits  of iron in  the basins of  the springs.  A seeping  carbonated
            spring issues  in  a  branch gully  about  150  yards  above  the principal
            drinking springs,  and  50  yards  farther up  the  main  ravine  the fifth
            spring  issues  from  a  bank  of  sandstone.  Like  the  two  principal
            springs,  this  spring  deposits  considerable  iron,  and,  like  the  lowest
            one, it deposits also small amounts of lime carbonate.  The water of
            all of the springs is  cool, and the flows  are  only a  quarter of a gallon
            to 2  gallons a minute.
                   SALMON  CREEK  MINERAL  SPRINGS  (MENDOCHSTO  18).
              A small camping resort has been built up at Salmon Creek Mineral
            Springs  about  12  miles  east  of  Willits.  Two  small  mineralized
            springs  on  the  property  are  known,  respectively,  as  Black  Sulphur
            and Soda and Iron, and are used during the camping season as  drink-
           ing springs.  They are similar in mode of occurrence to Baker Mineral
           Springs,  a few miles northward, but the sulphureted nature of one of
            the  springs  makes  it  similar in  general  character  to  springs  farther
           west on a branch of Deep Creek, which are described with the sulphur
           springs  (p.  258).

             CARBONATED  SPRINGS  AT  TRAVELERS  HOME  (MENDOCDSTO  13).
              At Travelers Home  (Hearst post office), which is  a small mountain,
           resort  14  miles by road northeast of Willits,  there are  about a dozen
           small carbonated springs.  Several of them are used for drinking, but
            they have not been  otherwise  developed.  The locality,  like  that of
            the other carbonated springs in the mountains eastward from Willits
           Valley, is one of disturbed sedimentary rocks.

                        KENSNER  SODA  SPRING  (MENDOCINO  14).
              Kinsner Soda Spring rises in  a ravine 150 yards south of the wagon
           road and  a mile west of Travelers Home.  The water, which rises in
           a  small  basin  excavated  in  soft  sandstone,  is  strongly  carbonated
           and probably contains  considerable calcium,  for lime  carbonate  and
           cemented gravel line portions of the bed of the ravine.  At the road-
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