Page 247 - 1915, Springs of CA.
P. 247

CARBONATED  SPRINGS.                   229

     them  had  an  appreciable  flow.  Each  of  these  yielded  perhaps  1
     gallon a minute.  One of them issued horizontally, with considerable
     force,  among lime-cemented  bowlders  at the  creek  side.  The  small
     flow is worthy of remark in connection with the size of the deposit.
       The  rocks  of  this  region  are  slates  and  sandstones,  with  some
     quartzitic  material,  that are very probably  of  the same  series  that
     has been mapped by Diller,1  3  or 4  miles westward,  and by Turner,2
     2  or 3  miles southward, as  the Calaveras formation,  of Carboniferous

       Although no lava was  observed near the springs,  the southeastern
     border of  the lava area that surrounds Lassen Peak is only about 10
     miles  to  the  west.  The  massive  and  hoodoo-like  character  of  the
     underlying portion of .the deposit makes it seem not improbable that
     the  springs  were  thermal  and  accomplished  most  of  their  work of
     deposition during or shortly following the eruptions from Lassen Peak,
     and  that  they represent one  phase of  the results of  volcanic activity
     when that mountain was in the making.
                     ARLINGTON  SPRINGS  (PLTTMAS  12).
       There  are  two  carbonated  springs  near  the  Arlington  Bridge,  at
     the  southeastern  edge  of  Indian  Valley,  3J  miles  in  a  direct  line
     northwest  of  the  carbonated  springs  on  Indian  Creek.  One  of  the
     Arlington Springs,  as  they are locally known  (though the name Bach
     Springs has also been applied to  them), rises in a barrel at the road-
     side;  the other issues from a short piece of  1-inch pipe,  on  the gentle
     hill slope  25  yards to  the southeast.  Both yield cool, pleasantly car-
     bonated water.  The following partial analysis shows the water to be
     chiefly of secondary alkaline character:

         Analysis of water from main spring,  Arlington Springs, Plumas  County,  Cal.
       [Analyst, G. E. Colby (1906).  Authority, owner of springs.  Constituents are in parts per million.]

     Properties of reaction:
                                                                   10
       Secondary salinity ..............  ................  ..............................  0
                                                                    0
                                                                    3
                                                                   87
                                                             ( f)
                                                          By   Reacting
                          Constituents.
                                                         weight.  values.
                                                        |   235  11.77
     Iron (Fe). ...........................................................................  Small.  Small.
     Sulphate (SO4). .....................................................................  33  .69
     Chloride(Cl). .......................................................................  23  .66
     Carbonate (CO3)...... . ..............................................................  365  12.18
                                                            100
     Silica (SiO2). .. . .....................................................................  Small.  Small.
                                                            799
     Carbon dioxide (CO2) ...............................................................
            1 Diller, J. S., U. S.  Geol. Survey Geol. Atlas, Lassen Peak folio (No.  15),  1895.
            2 Turner, H. W., U. S.  Geol. Survey Geol. Atlas, Downieville folio (No. 37), 1897.
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