Page 224 - 1915, Springs of CA.
P. 224

206                  SPRINGS  OF  CALIFORNIA.
           gentle slope  at the eastern base of  a brushy mountain and  are about
           10  miles  by  road  westward  from  Stonyford,  across  a  mountain
           divide.  In  1910  about  30  cottages,  a  dozen  tents  and  a  building
           containing  an  office  and  a  dining  hall,  furnished  accommodations
           for  150 guests.
             There  are  four  principal  springs  on  the  property.  Champagne
           Spring, which is the one most used for drinking, rises in a pool beneath
           the floor  of  a  spring house  near  a  small  creek  and  about  175  yards
           southwest  of  the  dining  hall.  It yields  a  small  flow  of  pleasantly
           carbonated  water  that  is  much  appreciated  for  drinking.  The
           analysis  shows  it to  be  a  moderately  mineralized  water,  secondary
           alkaline in character, markedly different from the waters of  the other
           two  springs  that  have  been  analyzed.  In  the  creek  bed,  about 20
           yards  south  of  the  spring, carbonated  water issues with much bub-
           bling, but in  1910 these springs had not been improved nor used.
             The three  other springs,  or groups  of springs,  are in  a ravine  one-
           half  to  three-fourths mile northwest of  the resort grounds.  Redeye
           Spring receives  its  name  from  the  rusty-red  stain  of  iron  along  its
           overflow  channel.  The  water  issues  from  seams  in  the  rock  on  the
           north bank of the creek,  where two small basins yield about one-half
           gallon and 5  gallons a  minute  of  carbonated  saline water that has a
           temperature of 75°.  This water was formerly bottled and  marketed
           and  is  still  used  for  drinking,  but,  as  is  shown  by  the  analysis,  it
           is  too  salty  to  be  pleasant  to the taste.  Many  bubbles  that rise  in
           the creek near Redeye Spring show that gas and probably also carbon-
           ated water issue from other seams in  the rock at this place.
             The Bath or New Life Spring is about 175 yards westward, upstream,
           from  Redeye  Spring and  on  the  same  side  of  the  creek.  The  main
           flow  comes  from  a  pool  2  feet  in  diameter,  which  yields  about  8
           gallons  a  minute,  and  a  small  pool  3  yards  away  yields  perhaps
           one-half  gallon  a  minute  more.  The  water  has  a  temperature  of
           75° and  tastes moderately carbonated and salty, like  that of Redeye
           Spring,  which  analysis  shows  it  to  closely  resemble,  both  being
           primary saline  and  secondary  alkaline  in  character,  but it has  built
           up a terrace of gravel and lime carbonate about 5  yards wide and 20
           yards  long  at  the  side  of  the  creek.   The  water  is  conducted  in
           a  trough  eastward  to  a  bathhouse  a  short  distance  below  Redeye
           Spring and  heated  for bathing.  It deposits much calcium carbonate
           in  the  trough,  though  the  following  analyses  show  that  it  contains
           the  least  calcium  of  the  three  spring  waters.  Noteworthy  features
           of  the  waters  shown  by  the  analyses  are  the  amounts  of  iodine,
           ammonium,  and  nitrate.
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