Page 281 - 1915, Springs of CA.
P. 281

SULPHUR  SPEINGS.                   261

     most  of  which  contains  glaucophane,  then  appears  as  the  road  is
     followed  southeastward  up  a  steep  grade  nearly  to  Kneeland  post
     office, which is about 20 miles from Eureka.  Chert is exposed at this
     place  and  extends,  interspersed  with  a  few  areas  of  serpentine,
    southeastward  nearly  to  Mountain  View  Spring.  The  spring
     issues  in  an  area  of  andesitic  lava,  which  is  exposed  on  the  lower
    slopes near the resort.  Serpentine appears above the andesite, on the
     slopes  across the creek  and  a short  distance southeast of  the spring,
     and  tremolite  schist  was  observed  still higher up  the hillside.

                      COOK  SPEING  (HUMBOLDT  4).
       Cook  Spring  is  about  7  miles  south  of  Mountain  View  Spring
     (Humboldt 3, p. 160), or 35 miles by road southeast of Eureka.  It is
     situated  near  the  north  bank  of  North  Yager  Creek, and  10  yards
     below the road, near the point at which the road crosses the stream a
     quarter of  a  mile  east  of  laqua.  A pool  14  inches in diameter here
     forms  a  drinking  basin  that  is  used  occasionally  by  travelers  and
     by the cattle of the surrounding range.
       Several  other  sulphur  springs  of  small  flow  issue  in  the  upper
     portions of the basin of North Yager Creek, but they are unimproved
     and  are  even  less  important  than  Cook  Spring.  ,A  small  sulphur
    spring  at  Felts  Springs  (Humboldt  5,  p.  300) is  mentioned  in  the
     description of  the saline springs  at that place.
       The  southern  boundary  of  the  andesite  along  the  road  from
    Mountain View Spring to Cook Spring is  about 2  miles south of  the
     former  place.  Mica  schist  that  contains  glaucophane  extends from
     that point to and beyond  Cook  Spring and  also westward  along the
    road  to  a  point  about  6  miles  in  a  direct  line  east  of  Fortuna.
    Unaltered  sediments  extend  from  this  point  northwestward  to the
     coast.  In the  schist  there  are  lenses  of  limestone,  and  many small
    sink holes have been formed by the partial solution and  removal  of
     this  material.
                     DEERLICK  SPRINGS  (TRINITY  3).
       Deerlick Springs are situated in the deep, rugged canyon of Browns
    Creek,  28  miles  by  road  and  trail  south  of  Weaverville.  They  are
     also  reached  by  9  miles  of  trail  northward  from  the  Midas  mine
    in Harrison Gulch  (Knob post office).  They have long been known
     as Coumbs Springs and have been a local camping resort.  A supply
    store  was  formerly  conducted  during  the  summer  in  a  cabin  that
     was  built  near  the  springs  more  than  20  years  ago.  During  1909
     the  property  changed  hands,  and  the  present  name  was  adopted.
       There  are  five  strongly  sulphureted  springs  on  the  property,  all
     on  the west  side  of  the  creek.  Two  of  them,  known  as  the  Blue
   276   277   278   279   280   281   282   283   284   285   286