﻿104 
  

  

  NEW 
  YORK 
  STATE 
  MUSEUM 
  

  

  370' 
  

  

  260' 
  

  

  165' 
  

  

  50' 
  

  

  40' 
  

  

  c 
  

  

  110' 
  

  

  95' 
  

  

  115' 
  

  

  10' 
  

  

  40' 
  

  

  SECTION 
  NORTH 
  OF 
  HARPERSVILLE 
  

   LXX 
  A 
  

  

  •A 
  6 
  Covered 
  nearly 
  to 
  the 
  top 
  of 
  the 
  hill 
  

  

  A 
  5 
  Sandstones 
  and 
  shales 
  for 
  most 
  of 
  the 
  distance 
  

   along 
  the 
  run 
  

  

  A 
  4 
  Covered 
  

  

  A 
  3 
  Sandstone 
  with 
  shale 
  at 
  base 
  

  

  A 
  2 
  Covered 
  

  

  A 
  1 
  Olive 
  shales 
  

  

  Creek 
  level 
  above 
  railroad 
  bridge 
  

  

  The 
  divide 
  between 
  the 
  Susquehanna 
  and 
  Chenango 
  rivers 
  

   which 
  crosses 
  the 
  western 
  central 
  part 
  of 
  Colesville 
  township 
  

   from 
  north 
  to 
  south 
  is 
  quite 
  heavily 
  covered 
  by 
  drift 
  so 
  that 
  

   outcrops 
  of 
  rocks 
  are 
  rather 
  infrequent; 
  but 
  along 
  the 
  streams 
  

   on 
  the 
  western 
  side 
  are 
  occasional 
  exposures; 
  those 
  in 
  the 
  vicinity 
  

   of 
  Osborne 
  Hollow, 
  near 
  the 
  western 
  line 
  of 
  Colesville 
  township, 
  

   were 
  described 
  in 
  part 
  1 
  of 
  this 
  report 
  , 
  and 
  to 
  the 
  west 
  near 
  the 
  

   top 
  of 
  the 
  high 
  hill 
  south 
  of 
  the 
  Chenango 
  river 
  below 
  Port 
  Crane 
  

  

  a.l5th 
  an. 
  rep't 
  N. 
  Y. 
  state 
  geologist, 
  p. 
  160-62. 
  

  

  