Page 128 - 1915, Springs of CA.
P. 128

120                 SPRINGS  OF  CALIFORNIA.
             This analysis probably also represents the general character of the
           springs of Hot Creek and also of Kellys Hot Spring.
                WARM  SPRINGS  NEAR  RATTLESNAKE  CREEK  (MODOC  8).
             Warm  springs  that  are  similar  to  those  of  Hot  Creek  and  Warm
           Spring Valley issue  along  the slopes  that border Rattlesnake Creek,
           about 7  miles above its junction with Pit River and 8  or 9  miles  (by
           road)  northwest  of  Alturas.  They  form  a  small  area  of  natural
           meadow land but have not been developed so as to water it efficiently.

                 WARM  SPRINGS  NEAR  CANYON  CREEK  (MODOC  7).
             Near the head  of Canyon  Creek,  south  of the valley of Pit River,
          warm  springs  that  are  similar  in  character  to  those  already  men-
           tioned in this region are used to irrigate a small amount of land on a
          ranch.
             The  region  including  the  five  groups  of  thermal  springs  last  de-
          scribed  forms  a  rather  mountainous  plateau  covered  with  lava.
           Faults  near  the  springs  are  not  mapped  on Plate  III  (in  pocket),
          but crustal movement is  suggested  by  the  unusually  high  tempera-
           ture of Kellys Hot Spring, and the rise of heated waters at this and the
           other  thermal  springs of  the region  may perhaps  be ascribed  to the
          heat of the lavas themselves.
                        KLAMATH  HOT  SPRINGS  (SISKIYOU  7).
             Klamath  Hot  Springs  form  an  isolated  group  near  the  north-
          central edge of the State.  The springs rise in meadow land that bor-
          ders  Klamath River near  the mouth  of Shovel Creek  and were  for-
          merly known as Shovel Creek Mud Springs.  The property has been
          improved as a resort for more than 20 years and is much visited for
           the  fishing  that is  afforded  by  the  river,  as  well  as  for  the  benefit
          derived from the baths.  In 1909  the improvements included a two-
          story  stone  hotel  (PL  VII,  B,  p.  108)  and  four  cottages,  besides
          bathing facilities.
             Five springs and tule-grown pools are formed by the rise of thermal
          water in a meadow on the south side of the river, and two other small
          springs issue  near  the northern bank  of  the stream.  Three springs
          on the southern side are those chiefly used.  The hottest of these, 152°
          in temperature, forms a small drinking spring near the river and about
           175 yards from the hotel.  There is a small bathhouse at another hot
          spring near by, and the main bathhouse is  100 yards to the southwest,
          at the border  of  a  tule  area.  Hot-mud  baths  and  also  clear-water
          baths are here furnished by water that rises in the marshy area.  The
          following are analyses of the main drinking and bath springs:
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