Page 7 - 1915, Springs of CA.
P. 7

SPRINGS  OF  CALIFORNIA.



                           By GERALD A. WARING.


               PHYSICAL  FEATURES  OF  CALIFORNIA.
                            NATURAL  DIVISIONS.
         As  a basis for the discussion of springs  and spring waters of Cali-
      fornia  a  brief  outline  of  the  physical  features  of  the  State is  here
      presented,  together  with  a  few  notes  on  the character  of  the rocks
       and  their  structure.  Such  an  outline  will  in  a  measure  serve  to
       explain the topographic and  geologic  maps  (Pis. I and II, in packet)
       and will indicate in a general way the relations of the facts shown on
       these maps to the various springs.
         Five  main  physiographic  provinces  may  be  recognized  in  the
      State:  (1)  The Coast  Ranges,  (2)  the  Great Central Valley,  (3)  the
      lava-covered region of the northeast,  (4)  the Sierra Nevada,  and  (5)
      the southeastern  desert region.  Not  all  of  these  provinces  are  dis-
      tinctly separated from one  another; neither do  they consist entirely
      of  marked  topographic  or structural features;  but  they form  fairly
      well-defined  natural divisions  that  are  convenient  in  discussing  the
      general features of the State.

                              COAST  RANGES.
        The term "Coast Ranges" is used in the present paper to designate
      the  system  of  mountain ranges  between  the  Great  Valley  and  the
      Pacific,  to  which  the  term  "Coast  Range"  has  been  applied,  with
      different limitations, by several geologists.1  In general, these ranges
      lie approximately parallel to the coast, but in the areas of more com-
      plex  structure  a  few  trend  in  other  directions.  To  the  ridges  or
      groups  that  make  up  the  system  many  names  have  been  applied.
      The range in the extreme northwestern part of  the State, forming the
      divide between the Smith and Klamath River basins and the bound-
       ary between Del Norte  and  Siskiyou  counties, is called the Siskiyou
      Mountains, and the mountains that extend eastward along the course
      of  Klamath  River are also  considered a part of  the Siskiyou MOUD-

        1  See Fairbanks, H. W., Review of our knowledge of the California Coast Ranges:  Geol. Soc. America
      Bull., vol. 6, pp. 73-75,1894.  Lawson has used the term "Coastal system" in speaking of the main por-
      tions of the Coast Ranges, in the report of the California Earthquake Investigation Commission (The Cali-
      fornia earthquake of Apr. 18,1906, vol. 1, pt. 1, p. 5).
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