Page 355 - 1915, Springs of CA.
P. 355

MINOR  PERENNIAL  SPRINGS.               835

                        MUD  SPRING  (TEHAMA  6).
      A few small springs form watering places near the western base of
    the  Sierra,  on  the slopes  of  tuffaceous  lava  that  border  Sacramento
    Valley in eastern Tehama County.  Mud Spring rises in a rock-walled
    pool,  6  feet in diameter,  at the northern edge of the county road,  13
    miles  north  of  east  from  Red  Bluff.  Its  water  has  been  piped  200
    yards  westward  to  a  watering  trough  near  sheepmen's  corrals  and
    camp,  where  the measured flow was  about one-half gallon  a minute.
                       GEARY  SPRING  (TEHAMA  7).
      Geary  Spring  is  similar  to  Mud  Spring  in  character.  It is  about
    7  miles  farther south  at  the side of  a small  drainage  channel in  the
    gentle, plateau-like slope.  The water rises 50 yards south of a wagon
    road, in a rock-curbed pool, 3 feet in diameter, that is used as  a water-
    ing and camping place by travelers and stockmen.
      The water of  Geary  and Mud springs is  of good  quality,  and their
    observed temperatures, which were respectively 66°  and 62°, suggest
    that it rises  from  a  depth  of  several  hundred  feet,  probably from  a
    layer in the bedded volcanic tuffs.

                     HENDERSON  SPRING  (BTTTTE  1).
      Henderson Spring issues from a steep  bank of slate, in the bottom
    of  the  canyon of  Big Butte Creek,  11  miles  by road  and  trail,  north
    of Stirling City.  The water is said to have  medicinal  properties and
    has been used for a number of years by several residents of the region,
    but in the fall of  1909  no mineralization was  noticeable to  the taste.
    At  this time,  however,  the water was  diluted  by storm  water.  The
    spring is  not  easy  of  access,  as  the  canyon is  steep  and  only  a  dim
    trail leads  from prospectors'  cabins  on  its  upper slopes  down  to  the
    creek and the spring.
                      BLACK  SPRING  (MARIPOSA  1).
      In  Yosemite  Valley  there  are  several  perennial  springs  of  cold
    water,  of  which  Black Spring is perhaps the best known.  It issues
    on the slopes on  the northern side of the stage road, 4f miles south-
    west of Yosemite post office,  and is piped  to  the  roadside,  where it
    forms  a  watering  place  for  horses  as  well  as  people.  The  water  is
    cold  and of excellent quality.
                      MOSS  SPRING  (MARIPOSA  3).
      Moss Spring issues on the southern side of Yosemite Valley,  about
    one-third  of  a  mile  south  of  Black  Spring,  in  the lower  land  at  the
    base  of  the  valley  wall.  It is  similar  in  character  to  Black Spring,
    but as it is not beside a main road its water has been little used.
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