﻿B! 
  STORE 
  STATE 
  M( 
  si.i 
  \i 
  

  

  conformably 
  inverted. 
  «>n 
  account 
  of 
  their 
  beina 
  

   the 
  remnant 
  of 
  the 
  underturned 
  wing 
  of 
  an 
  overturned 
  fold 
  of 
  

   Appalachian 
  type. 
  Thia 
  fold 
  has 
  turned 
  Into 
  an 
  overthrnst 
  

   fault, 
  which 
  brought 
  the 
  Cambric 
  beds 
  as 
  the 
  nexi 
  succeeding 
  

   terrane 
  above 
  the 
  Normans 
  kill 
  8hal< 
  

  

  ( 
  '>< 
  a 
  count 
  of 
  the 
  fact 
  that 
  the 
  mass 
  of 
  beds 
  hitherto 
  called 
  

   Hudson 
  river 
  shales 
  and 
  correlated 
  with 
  the 
  Lorraine 
  beds 
  of 
  

   central 
  v 
  u 
  Fork, 
  i> 
  composed 
  of 
  terranes 
  ranging 
  from 
  the 
  Lor- 
  

   raine 
  to 
  the 
  lower 
  Trenton, 
  ami 
  on 
  account 
  of 
  the 
  lack 
  of 
  a 
  fullv 
  

  

  • 
  

  

  representative 
  fauna 
  and 
  of 
  a 
  complete 
  section 
  of 
  the 
  Lorraine 
  

   portion 
  of 
  these 
  terranes, 
  it 
  is 
  proposed 
  to 
  drop 
  the 
  term. 
  "Hudson 
  

   - 
  . 
  for 
  the 
  uppermost 
  part 
  of 
  the 
  Lower 
  Siluric, 
  and 
  

   the 
  term, 
  "Hudson 
  river 
  group", 
  for 
  the 
  Utica 
  and 
  Lorraine 
  beds, 
  

   and 
  to 
  employ 
  the 
  term 
  Normans 
  kill 
  shales 
  for 
  the 
  clastic 
  facies 
  

   of 
  a 
  part 
  of 
  the 
  lower 
  Trenton 
  which 
  is 
  characterized 
  bv 
  the 
  

   dite 
  fauna 
  at 
  the 
  Normans 
  kill. 
  

  

  