﻿EEPORT 
  OF 
  THE 
  DIRECTOR 
  rlOl 
  

  

  west 
  in 
  the 
  vicinity 
  of 
  Yictor, 
  where 
  the 
  kames 
  have 
  been 
  partially 
  

   lieveled 
  by 
  the 
  static 
  waters 
  and, 
  from 
  this 
  point 
  eastward, 
  an 
  

   abundance 
  of 
  sand 
  and 
  silt 
  deposits 
  are 
  found 
  scattered 
  over 
  the 
  

   plain 
  skirting 
  the 
  northern 
  end 
  of 
  the 
  Finger-lakes. 
  

  

  Warren 
  lake 
  stage 
  

   Markings 
  of 
  lake 
  level 
  : 
  

  

  Owasco 
  lake 
  valley 
  

  

  Casowasco 
  creek. 
  822 
  feet. 
  832 
  feet. 
  

  

  Kexbka 
  laTce 
  valley 
  

  

  Locke. 
  865 
  feet. 
  

  

  Moravia. 
  880 
  feet. 
  850 
  feet. 
  

  

  Urbana. 
  840 
  (?) 
  feet. 
  

  

  Canandaigua 
  lalce 
  valley 
  

  

  Parrish 
  gnlly. 
  845 
  feet. 
  

  

  Cayuga 
  lake 
  valley 
  

  

  Butternut 
  creek. 
  800 
  feet. 
  845 
  feet. 
  

  

  Woodcock 
  stream. 
  890 
  feet. 
  

  

  West 
  branch. 
  825 
  feet. 
  

  

  Coy 
  glen. 
  804 
  feet. 
  826 
  feet. 
  864 
  feet. 
  

  

  Taughannock. 
  804 
  feet. 
  834 
  feet. 
  '^ 
  843 
  feet. 
  

  

  Trumansburg. 
  807 
  feet. 
  827 
  feet. 
  868 
  feet. 
  

  

  Buttermilk. 
  S. 
  side, 
  800 
  feet. 
  892 
  feet. 
  N. 
  side, 
  834 
  feet. 
  

  

  Yan 
  Buskirk. 
  816 
  (h) 
  feet. 
  826 
  (h) 
  feet. 
  836 
  feet. 
  

  

  Seneca 
  lake 
  valley 
  

  

  Watkins. 
  803 
  feet. 
  

  

  Big 
  stream. 
  830 
  feet. 
  880 
  feet. 
  

  

  Ilimrods. 
  842 
  feet. 
  

  

  Havana. 
  837 
  feet. 
  

  

  Lodi. 
  840 
  feet. 
  

  

  Burdett. 
  818 
  feet. 
  898 
  feet. 
  

  

  Evidence 
  and 
  history 
  of 
  lake. 
  The 
  next 
  and 
  last 
  stage 
  traced 
  

   in 
  the 
  history 
  of 
  the 
  Finger-lakes 
  was 
  connected 
  with 
  the 
  Warren 
  ^ 
  

  

  a 
  Accurately 
  measured 
  with 
  an 
  engineer's 
  level 
  and 
  rod. 
  

  

  h 
  This 
  name 
  was 
  first 
  proposed 
  by 
  J. 
  W 
  Spencer 
  in 
  Science 
  1888, 
  11, 
  p. 
  49. 
  For 
  a 
  description 
  

   of 
  its 
  extent, 
  etc 
  , 
  see 
  articles 
  by 
  Spencer, 
  J. 
  W. 
  , 
  Taylor, 
  F. 
  B., 
  Upham, 
  W., 
  and 
  others 
  in 
  

   Bull. 
  G 
  S. 
  A., 
  Am. 
  jo. 
  sci., 
  and 
  Am. 
  geol. 
  

  

  (h) 
  Indicates 
  a 
  slight 
  halt 
  in 
  the 
  waters, 
  marked 
  by 
  slighter 
  delta 
  forms. 
  

  

  