Page 374 - 1915, Springs of CA.
P. 374

354                 SPRINGS  OP  CALIFORNIA.

           and the water is piped a few yards to a board-curbed pool  that forms
           a watering place for cattle.  In July,  1909,  the visible flow was about
           1  gallon a minute of water of good quality.
                     SPRINGS  NORTHWEST  OF  ROSAMOND  (KERN  24).
             Springs that are similar to the one just described issue a mile north-
           eastward  and  higher  up  on  the  slope.  They  have  been  used  as  a
           water-supply point and a camping place by prospectors.  The water
           issues  at  two  points  a  few  yards  apart  on  a  gentle  slope  that  rises
           northward  to  steep hills.  One spring seeps  from beneath  a ledge  of
           tuffaceous  material.  The  other  issues  in  a  small  excavation  and
           forms a pool behind a cement dam.  Each spring yields perhaps one-
           half gallon a minute of water of good quality.
             The  hills  north  of  these  springs  are  composed  partly  of  volcanic
           material,  and  the  water  seems  to  issue  from  a  porous  tuffaceous
           layer.  These springs, however, like Willow Springs (Kern 22, p. 318),
           which  have  been  described  among  the  artesian springs,  issue  at  the
           upper edge of  a gentle slope that lies between a flat valley'and steep
           hills, and the water may rise along a small fault that borders the valley.
                        SPRINGS  ON  TEMBLOR  RANCH  (KERN  4).
             In the Coast Ranges  that lie  along the southwest side of San Joa-
           quin Valley there are a number of perennial springs that resemble in
           general character those in the southeastern part of the State, for they
           are in an arid region,  are of small flow,  and are of importance mainly
           because they form watering places.  Those which  are in the eastern,
           portion of San Luis  Obispo  County'and  the western portion of Kern
           County have been of value as watering places for range cattle as well
           as  for  travelers,  however,  so  have  been  more  often  used  than  those
           in  the  southeastern  desert  region.  The  water  of  most  of  them  is
           notably brackish or bitter, and a number of them are also sulphureted.
           One strongly sulphureted spring  (San Luis Obispo  12,  p. 277), that is
           used  to  supply  cattle-watering  troughs,  has  been  described  among
           the sulphur springs.  Springs  that rise on  the Temblor ranch/about
           12  miles  northwest  of  MeKittriek,  yield  a  supply  of  water  that  is
           sufficient for a small amount of irrigation.  The water is not of very
           good quality, however,  being noticeably hard.

                       THOMPSON  SPRING  (SAN  LUIS  OBISPO  6).
             Thompson Spring is in Carrizo Plain, westward across the Temblor
           Range  from  McKittriek.  The  spring  rises  in  a  curbed  pool  about
           8  feet  square  and  6  feet  deep,  at  the  base  of  a  knoll of  clay  and
           gravel.  It yields about 2 gallons a minute of slightly brackish water,
           which is  piped  to  a  cattle trough  near by.  Two smaller springs are
   369   370   371   372   373   374   375   376   377   378   379