﻿1 
  84 
  

  

  NEW 
  YORK 
  STATE 
  MUSEUM 
  

  

  that 
  are 
  bounded 
  by 
  one 
  fault 
  and 
  (b) 
  those 
  that 
  lie 
  between 
  two 
  

   faults 
  (ihorst). 
  We 
  have 
  good 
  examples 
  of 
  both 
  kinds 
  in 
  this 
  

   State, 
  at 
  the 
  hand 
  of 
  which 
  we 
  will 
  note 
  their 
  general 
  characters. 
  

  

  Fig. 
  24 
  Ohio 
  basin 
  with 
  the 
  Cincinnatti 
  and 
  Nashville 
  inliers 
  

   Siluric; 
  

  

  ^ 
  

  

  Upper 
  Siluric; 
  

  

  Devonic; 
  

  

  Lower 
  

  

  Mississippian; 
  

  

  Pennsylvanian. 
  Scale 
  

  

  The 
  best 
  ones 
  are 
  furnished 
  by 
  the 
  Mohawk 
  valley, 
  which 
  is 
  

   crossed 
  by 
  a 
  system 
  of 
  northeast 
  striking 
  faults, 
  mostly 
  with 
  the 
  

  

  