﻿i 
  BEUM 
  

  

  mentiona 
  among 
  the 
  localities 
  <»r 
  the 
  [Jtica 
  Bhale 
  mk-Ii 
  typi- 
  

  

  Electing 
  grom 
  the 
  Normans 
  kill 
  fauna 
  as 
  the 
  banks 
  

  

  B 
  kill 
  itself, 
  the 
  Kinderbook 
  creek 
  and 
  the 
  city 
  of 
  

  

  Ho 
  li 
  l 
  by 
  ili«' 
  Bnpposed 
  Identity 
  of 
  the 
  two 
  graptolite 
  

  

  8 
  which 
  later 
  were 
  se] 
  I 
  b\ 
  Hall, 
  he 
  considered 
  the 
  

  

  mans 
  kill 
  shales 
  as 
  homotaxial 
  with 
  the 
  Utica 
  Bhale. 
  This 
  

  

  UI 
  aceptioD 
  has 
  apparently 
  mislead 
  still 
  later 
  writers. 
  

  

  Lardner 
  Vanuxem 
  

   Lardner 
  Vanui 
  . 
  like 
  all 
  the 
  members 
  of 
  the 
  Bnrvey, 
  ac- 
  

  

  •d 
  Mather's 
  term 
  and 
  called 
  all 
  the 
  beds 
  between 
  the 
  Utica 
  

   shale 
  and 
  the 
  gray 
  Bandstone 
  of 
  Oswego, 
  the 
  Hudson 
  river 
  group, 
  

   l>m 
  pointed 
  out, 
  thai 
  there 
  are 
  two 
  divisions 
  which 
  are 
  not 
  coex- 
  

   tensive, 
  embraced 
  by 
  ibis 
  term, 
  namely, 
  a 
  lower 
  one 
  (the 
  Frank- 
  

   fort 
  si; 
  s 
  which 
  passes 
  from 
  the 
  Hudson 
  valley 
  through 
  the 
  

   ■auk 
  valley 
  and 
  extends 
  north 
  by 
  Rome 
  through 
  Lewis 
  county 
  

   i 
  Jefferson 
  county; 
  and 
  an 
  upper 
  division 
  (the 
  Pulaski 
  shale), 
  

   which 
  first 
  appears 
  in 
  Oneida 
  county 
  and 
  extends 
  from 
  thence 
  

   uunh 
  •' 
  in 
  ' 
  1 
  w«rt. 
  1' 
  iv 
  pare 
  in 
  the 
  Frankfort 
  slate, 
  but 
  are 
  

  

  numerous 
  where 
  ii 
  joins 
  the 
  next 
  series, 
  the 
  Pulaski 
  beds. 
  They 
  

   have 
  been 
  reported 
  from 
  near 
  Rome, 
  Westmoreland 
  and 
  Utica, 
  

   and 
  also 
  from 
  Oohoes 
  Bear 
  Waterford^ 
  though 
  the 
  species 
  are 
  not 
  

  

  •d. 
  

  

  I 
  ia 
  obvious 
  that 
  Vanuxem 
  correlates 
  only 
  the 
  lower 
  or 
  Frank- 
  

   with 
  the 
  beds 
  of 
  the 
  Hudson 
  valley. 
  

  

  Ebenezer 
  Emmons 
  

  

  lu 
  ?1 
  " 
  i 
  Bmmona 
  (3) 
  described 
  shales 
  of 
  the 
  Hudson 
  

  

  val 
  3 
  :! 
  "' 
  ,l 
  " 
  iea 
  or 
  group 
  and 
  Btated 
  their 
  exten- 
  

  

  through 
  New 
  Fork 
  and 
  Vermonl 
  to 
  Quebec 
  and 
  

  

  - 
  Pennsylvan 
  e 
  ►uthern 
  -. 
  He 
  proposed 
  the 
  

  

  "Lorraine 
  shales" 
  in 
  place 
  of 
  the 
  names 
  ■• 
  Pulaski 
  shall 
  

  

  • 
  Hudson 
  river 
  shale," 
  ased 
  before, 
  on 
  the 
  -round 
  thai 
  at 
  

  

  1 
  >mplete 
  section 
  with 
  the 
  top 
  and 
  bottom 
  of 
  

  

  the 
  -""'J' 
  exposed, 
  could 
  be 
  found 
  (3:119). 
  This 
  term 
  has 
  

  

  ndancy 
  with 
  the 
  term, 
  Hudson 
  river 
  

  

  r 
  

  

  