Page 381 - 1915, Springs of CA.
P. 381

MINOR  PERENNIAL  SPRINGS.               361
      Mountain Springs,  6  miles west of Jackson in Amador County, and
    Valley  Springs,  at  the  terminus  of  the  railroad  10  miles  west  of
    San  Andreas  in  Calaveras  County,  are  at small settlements.  There
    are also saline springs near the latter place, which have already been
    described.  Cottage  Spring,  5  miles  northeast  of  Valley  Springs,
    has  been  locally  used  as  a  water  supply.  Another  Cottage  Spring
    and  Black  Spring  and  Hermit  Spring  are  near  the  road  that  runs
    northward from the north grove of  the Calaveras big trees, in north-
    eastern Calaveras County.
       Coif ax Spring, which is on the south edge of Tuolumne County, 25
    miles in a direct line southeast of Sonora, has given its name to a small
    settlement.  Gold Spring,  7  miles north of  Sonora,  arid Cold Spring,
    30 miles northeast of the same town,  are locally known.
      FrSmont Spring,  which is on the southeast slope of Bullion Moun-
    tains,  30  miles in  a  direct line northeast  of Merced,  is known to  the
    miners of the locality.  In the higher Sierra east of Merced there are
    a few  small  perennial  springs,  among the principal ones  being  Cold
    Springs,  between Mariposa  and the Mariposa Grove of big trees.  A
    few larger ones in the Sierra have been previously described.
      Numerous  cool  springs  of  perennial  flow  issue  along  the  north-
    western  border  of  Mono  Valley,  in  the  eastern  part  of  the  State.
    Several  of  them  afford  watering places  for range  cattle  and  horses,
     and a few irrigate small meadows,  but they have not been efficiently
    developed.  One that rises on the southern side of Mono Lake a short
    distance from the water's edge was formerly known as Blairs Spring.
    The water is noticeably calcic, but it has long been used as a drinking
    spring.  Other small springs rise in the lake and several of them issue
    from domes or crags of calcareous tufa that are built up from the lake
    bottom.  These  springs  have  been  mentioned  in  the  description  of
    Mono Basin Warm Springs (Mono 8, p. 145), and an analysis of water
    from  one  of  them  is  tabulated  with  that  of  water  from  the  warm
     springs.
       In the higher portions  of  the southern  Sierra  a few small springs
     form drinking places beside mountain trails.  Among them are Windy
     Springs, which are on a tributary of South Fork of Kern River, about
     13  miles  in  a  direct  line  southwest  of  former  Haiwee  stage  station
     (Inyo 26, p. 339);  Boulder Spring, which is 18 miles by trail southeast
     of  Onyx  post  office;  and  Bird  Spring,  which  is  20  miles  by  trail
     southeast  of  Weldon  post  office  and  6  miles  in  a  direct line  west  of
     Boulder Spring.
       Along  the arid southeastern portion of  the Sierra, southward from
     Haiwee  to  Mohave,  there  are  very  few  perennial  springs,  though
     seepage or underflow in Red Rock Canyon and farther south, at Water
     Station (Kern 21, ,p. 341), yields a fairly dependable supply.  South of
    Mohave, in the mountains bordering Antelope Valley, in whose basin
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