Page 101 - 1915, Springs of CA.
P. 101

HOT  SPRINGS.                       95
    other  radicles,  it  indicates  probable  contact  with  magnesium-rich
    rocks.  As its name implies, the Arsenic Spring contains an exception-
    ally large proportion of arsenic and its content  of  aluminum  is  also
    uncommon  for  an  alkaline  water.  All  the  springs  contain  iron  in
    unusual proportion.
      Shale  that  dips  at  steep  angles  is  exposed  on  the  hillsides  near
    Harbin  Springs,  but  about  25  yards  above  the  springs  a  belt  of
    amphibolite schist appears.  Its observed thickness is about 25 yards
    and  its lower side  apparently crosses  the ravine very near the point
    at  which  the springs  emerge.  As  the  high  tilting  of  the sediments
    is the only other  geologic  feature  noticed  that might account for the
    springs  at  this  place,  it  appears  probable  that  the  schist  at  least
    furnishes  a  point  of escape  for  deep waters, and it possibly also  aids
    in giving  the  water its abnormal  temperature.  The  conditions pre-
    sented  by  this  rock  cutting  through  the  sediments  just  above  the
    springs  may  be  similar  to  those  at  Mercey Hot  Springs, in  Fresno
    County.  (See p.  78.)

                      HOWARD  SPRINGS  (LAKE  51).
      About  9  miles  southwest  of  the  town  of  Lower  Lake  a  group  of
    mineral springs  (PL VI,  C, p. 92), several of which are notably warm,
    issue in a line about 50 yards long at the base of a slope that borders
    the south side of a drainage course.  A number of seepages have been
    dug  out  and  cemented  to  form  drinking  basins,  so  that  about  26
    improved  springs  may  be  counted,  although  the  group  is  said  to
    include 42 springs.  Of  the 8  springs that are of  chief  importance  5
    are  used  for  drinking  and  have  been  named  Bohemia,  Neptune,
    Lithia,  and  Magnesia  Twins.  They  have  observed  temperatures,
    respectively, of 66°, 70°, 73°, 71 °, and 100°.  When the writer visited
    it  in  1909,  Bohemia  Spring  discharged  about  1  gallon  a  minute,
    while the other three rose in basins from which there was no  appreci-
    able overflow.  The largest three springs are used mainly for bathing.
    Of these,  the Hot Soda or Hot Sulphur Spring has  a  temperature of
    110° and discharges approximately 125 gallons a minute into a plunge
    bath.  Excelsior  or Borax Spring,  with  a  temperature of  95°  and  a
    flow  of  perhaps  5  gallons  a  minute,  also  supplies  a  plunge  bath.
    Water  from  Eureka  Spring  is  piped  to  tub  baths,  its  temperature
    being  107°  and its  yield perhaps  2  gallons  a minute.  The  available
    analyses  of several  of  the springs  are here given  in  form convenient
    for comparison. 1
     i The analyses of  Lithia Spring and Bohemia Spring, published in advertising matter, have  not  been
    reproduced, as they appear to be incorrectly stated.
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