Page 390 - 1915, Springs of CA.
P. 390

370                 SPRINGS  OP  CALIFORNIA.

           north of the road summit and 25 yards from the road, there is another
           spring  that  has been improved by  a joint of  pipe  and a half barrel
           so  as  to  form  a  watering  place.  Both  of  these  springs  issue  from
           crushed and altered sediments that constitute the greater part of the
           rocks in this region.
             On  the  road  that leads  from  Bartlett  Springs (Lake 9,  p.  200)  to
           Crab tree  Springs  (Lake  5,  p.  106),  about  halfway  between  the  two
           places, on the grade north of Twin Valleys,  a spring that issues from
           altered sandstone and forms  a welcome  drinking pool yields  about 3
           gallons a minute of good water.
             Candybucket Spring is thus locally known because a candy bucket
           was for some  time kept near it for the use  of teamsters in watering
           their  teams  and  of  automobilists in replenishing their radiators.  It
           issues  at  the side  of  the road  between Stonyford  and Fouts Springs
           (Colusa 3, p. 205), about 3 miles east of the latter place and 100 yards
           north of the summit of the grade  between the two places.  It yields
           a summer flow of 2  or 3  gallons a minute,  but  the water issues  from
           altered sediments near an area of serpentine and is not very good.
             Rattlesnake  Spring is  at the roadside  about  6  miles  east of Alder
           Springs (Glenn 1, p. 359).  It yields a small flow that has been used as
           a roadside watering place, but it is of interest chiefly because water is
           not plentiful in the region.
             In  the  portions  of  the  Coast  Ranges  that  drain  into  northern
           Sacramento Valley water is much scarcer than it is farther southwest.
           Among the springs in the higher part of this region may be mentioned
           one  on  the  northern  side  of  Toms  Head  Mountain,  about  10  miles
           northwest of Colyear  Springs  (Tehama 10,  p. 266),  and another near
           the  county line,  about 8 miles farther northwest.  Near  the summit
           of the range, 25 miles farther  north, Kenshaw  Spring  issues about 6
           miles south of  Deerlick  Springs  (Trinity 3, p.  261).  A spring at the
           creek  edge one-half  mile south of Deerlick  Springs is of  interest be-
           cause of the coldness of its water, a temperature of 47° being recorded
           in summer.
             In  the  rugged  portions  of  Humboldt  County,  back  from  the
           coast,  there  are  several  nonmineral  springs,  and  a  few  that  are
           better  known  issue  in  the  less  sparsely  inhabited  section  along  the
           larger streams.  One  of  these  springs is  about 2  miles north of Mad
           River and 7 miles from the coast,  and a larger one issues a mile east
           of  Trinity  River  and  4  miles  south  of  the  northern  border  of  the
           county.
             In Del Norte County, which is in the northwest corner of the State,
           there are at least four springs of notable flow in the drainage basin of
           Smith River.  Two of these springs are on branches of the south fork
           of  the  river  and  are  respectively  about  17  miles  southeast  and  10
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