Page 330 - 1915, Springs of CA.
P. 330

310                 SPRINGS  OF  CALIFORNIA.

            The following analyses show that they are essentially primary saline
          and  secondary alkaline  waters,  the  upper  spring  having  the  higher
          salinity:
                 ArMlyses of water from  Mendenhall Springs,  Alameda  County,  Cal.
                              [Constituents are in parts per million.]
                                          1L          2            if

                                                                14° C .  (58° F.).
          Properties of reaction:
                                              35           31           42
                                               0           0            18
                                               0           0            0
                                               8           1            0
                                              57     (' 5  68           40
                                              54                        32
                                      By  Reacting   By  Reacting   By  Reacting
                   Constituents.
                                     weight.  values.  weight.  values.  weight.  values.
                                      136    5.91         4.16  148    6  43
                                       5.5    .14                    ^P-ra/Hi
                                       95    4.72  106    5.30  104    5.17
                                       41    3.36  44     3.61  46     3.77
                                       3.3    .37               3.6     40
          Sulphate (SO<)... . ........................  178  3.70  144  3  nn  37il  7.78
          Chloride (01)..............................  42  1.18  38  1.08  52  1.48
                                      278    9.25  97ft   Q  QQ  183   6.11
          Silica ( S iO 2) ...............................  7.2  .24  7.2  Q  i  .32
                                      786.0        705.2      '  920.0
                                      164    7.45               79     3.58
                                                                18     1.06
           1.  Lower Spring.  Analyst and authority, Winslow Anderson (1888).
           2.  Lower Spring.  Analyst, FaLkenau and Reese.  Authority, 8th Cal.
           3.  Upper Spring.  Analyst and authority, Winslow Anderson (1889).
            The  water is  apparently  of  surface  origin  and  has  become  some-
          what  mineralized  from  the  materials  through  which  it  percolates.
          The  tunnels  are  driven  into thin-bedded  cherts  and  crushed  shales
          that belong to the Franciscan group.
            The  property has been improved  as  a mountain resort for a num-
          ber of  years.  In  1909  accommodations for 75  people  were  provided
          by several cottages and by a dining room in the main building.
                           SWEET  SPRINGS  (ALAMEDA  6).
            Another  group  of  magnesic  springs  that  are  associated  with  ser-
          pentinous rock rise at the border of  a small meadow on  a low saddle
          between  two  ravines  18  miles  southeast  of  Livermore.  The  group,
          which is  known  as  Sweet  Springs,  includes  10  that issue for a space
          of 200 yards along the southern side of the meadow and 4 others that
          issue  on its  eastern side.  They range in size from mere seepages  to
          flows  of  6  or  8  gallons  a  minute,  the  total  yield  being  perhaps  30
          gallons  a  minute.  The  water  has  a  distinctly  sweet  taste.  The
          locality has been used by range stock as  a watering place.
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