Page 237 - 1915, Springs of CA.
P. 237

CARBONATED  SPRINGS.                  219
                    TABLE  BOCK  SPRING  (SISKtYOTT  9).
       Three  carbonated  springs  on  the  northeast  side  of  Shasta Valley
     may be considered  to  be in  the same general  locality as  those near
     Little Bogus  Creek.  The principal  one is  on  the Terwilliger ranch,
     12 miles east of Montague.  It is situated a few hundred yards north
     of Little  Shasta  River  and  near  the  northern  base  of  a  flat-topped
     hill known  as  Table  Rock.  During  1909  the  water  was  placed  on
     the market under the label ''Table Rock Water."
       At this  place  there is  a very low mound  of lime  carbonate about
     100  yards  in  diameter,  from  near  the  center  of  which  the  spring
     rises,  mainly  from  an  irregular  fissure  12  feet  long  and  1  inch  to
     30  inches  wide,  along  which  the  water  is  continuously  and  vigor-
     ously bubbling.  This fissure has been  protected by a concrete wall
     2^  feet  high.  In  a  bottling  house  beside  it water  for  bottling  has
     been obtained by a hand pump from a basin or well 1 foot in diameter
     and  10  feet  deep.  Near  the bottling  house  there is  also  a shallow
     bubbling  pond,  8  or  10  yards  across.  The  water  is  not  notably
     thermal, as it has a temperature of only 65°, but otherwise its occur-
     rence is similar to that of the springs near Little Bogus Creek.  It is
     more  strongly  carbonated,  however,  and  much  less  salty,  and  it
     probably contains  considerable iron,  as it deeply stains its  overflow
     channel.

     CARBONATED  SPRING AT EDGE  OF LITTLE  SHASTA RIVER  (SISEIYOTJ 8).
       Two  miles  downstream from  Table  Rock  Spring,  and half  a mile
     east of Little Shasta post office, strongly carbonated water rises from
     lava  gravel  at  the  southern  edge  of  Little  Shasta  River,  30  yards
     north of a low lava bluff.  The spring yields about 8 gallons a minute
     of  water,  57°  in  temperature.  It rises  clear  but is  said  to  become
     cloudy,  probably  from  a  small  amount  of  precipitated  iron,  after
     being bottled for a short tune.  Considerable iron-stained,  cemented
     gravel is exposed in a stream bank 50  to  100 yards above the spring,
     and  indicates  that  carbonated  water  formerly  issued  farther  up-
     stream.  The  spring  has  been  protected  by  a  short  piece  of  heavy
     galvanized-iron casing,  but it is in  pasture land some  distance from
     the road and has not been much used.

                   MARTIN  SODA  SPRING  (SISEIYOTT  11).
       The  third  of  the carbonated springs  near  Shasta  Valley issues  on
     the ranch of Mrs. M. F. Martin, near the southern base of Table Rock,
     about  a  mile  southward  in  a  direct  line  from  Table  Rock  Spring.
     The Martin spring rises in  a  cemented basin  at the edge  of  a  creek.
     Its water is  clear,  cool  (55°),  and strongly carbonated,  but its yield
     is only about  1  gallon a minute.  Like the water of the spring at the
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