﻿FIFTH 
  REPORT 
  OF 
  THE 
  DIRECTOR 
  I908 
  

  

  177 
  

  

  c 
  Glacial 
  erosion 
  inlicrs. 
  As 
  inliers 
  caused 
  by 
  glacial 
  erosion 
  

   we 
  consider 
  those 
  cases 
  where 
  in 
  the 
  Finger 
  Lake 
  region 
  an 
  

  

  Fig. 
  16 
  Sketch 
  map 
  of 
  " 
  Icy 
  Cove 
  " 
  from 
  Standingston*^ 
  

   folio, 
  Tenn. 
  Scale 
  ssion 
  

  

  Fio. 
  17 
  Geologic 
  mati 
  ( 
  f 
  ,"icy 
  Cove," 
  showing 
  the 
  

   Newman 
  limestone 
  I 
  I 
  forming 
  the 
  bottom 
  of 
  

  

  the 
  depression 
  and 
  the 
  Pennington 
  shale 
  ^:^;■•l^v.■v^- 
  

   following 
  formations 
  the 
  walls 
  

  

  and 
  

  

  