Page 380 - 1915, Springs of CA.
P. 380

360                  SPEINGS  OF  CALIFORNIA.
          ing  range  stock.  There  are  two  springs  at  the  locality,  but  their
          yield  is  small.  Coyote  Spring  is  about  12  miles  south  of  Moon
          Springs  and, like  them it yields  a small amount of water and is used
          by  range  stock.  Tadpole  Spring  is  on  the  southwestern  slopes  of
          Lassen  Peak  beside  the  stage  road,  3  miles  east  of  Paynes  Creek
          post office.  It yields a slight flow that is piped to a roadside watering
          trough, 100 yards to the northeast,  and to a house near by for domestic
          use.  The  water  issues  from  the  tuffaceous  material  known  as  the
          Tuscan  tuff,  the supply probably being derived from water  that col-
          lects in a porous layer of the material.  Springs are not plentiful in the
          lower slopes  of  the  lava  area  that surrounds Lassen  Peak,  so  those
          which exist are of local  importance.  On the higher slopes, however,
          water  is  more  plentiful  and  the  presence  of  small  springs  of  fresh
          water is  of  less  importance.
            In Plumas County,  on  the stage road between Quincy and Green-
          ville,  there  are  a  number  of  springs  that supply  roadside  watering
          troughs.  Their waters issue from slate and shale along the canyons
          of Spanish and Indian creeks,  and  they yield flows  of about 1  to  10
          gallons a minute.  Eight springs of cold nonmineral water that supply
          drinking pools or horse troughs were counted at the roadside along the
          canyons of  these creeks.  A number of cold springs issue in meadow-
          land  in  Grizzly  Valley,  about  12  miles  northwest  of  Beckwith,  and
          furnish a considerable part of the flow of Big Grizzly Creek.
            The  lower  portions  of  the  western  slopes  of  the  Sierra  contain
          relatively  few  perennial  springs.  Some  of  these  surface  springs
          were  early made use  of,  however,  by miners who  were working gold
          placer  gravels  and  ledges,  and  small  settlements  were  formed  near
          them.  Forest  Spring,  which  is  3  miles  south  of  Nevada  City,  and
          Indian Springs,  which  are 8  miles  southwest of  the same town, lent
          their names to mining settlements.  There are also several perennial
          springs in Eldorado County at places where mining camps were built
          up in the early days, but the springs are not now of great importance.
          Among  these are  Shingle,  Mud,  and Diamond springs,  near the rail-
          road  between  Sacramento  and  Placerville.  Several  other  springs
          afford watering places on a road between Placerville and Silver Lake,
          which  is  a  small  water  body  in  the  northeastern  corner  of Amador
          County.  Among them are Caple, Camp, Leek,  and Tragedy springs,
          which are respectively about 26, 30, 40, and 47 miles by road eastward
          from  Placerville.  All  yield  cold  water  of  good  quality  but  are  of
          small flow.  A few springs near the boundary between Eldorado and
          Amador  counties  are  also  of  some  importance  as  watering  places.
          Among  these  are  Marble,  Antelope,  and  Mud  springs,  which  are,
          in direct lines, respectively 22, 28, and 35 miles east of Latrobe station
          on the railroad to  Placerville.
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