﻿igo 
  

  

  NEW 
  YORK 
  STATE 
  MUSEUM 
  

  

  one 
  further 
  considers 
  that 
  the 
  former 
  series, 
  at 
  that 
  locaHty, 
  is 
  

   fully 
  undisturbed 
  and 
  the 
  other 
  abruptly 
  folded 
  in 
  closely 
  packed 
  

  

  Fig. 
  31 
  Shows 
  formation 
  of 
  inliers 
  by 
  overthrvists. 
  From 
  

   Rome 
  quadrangle 
  (Ga.— 
  Ala.). 
  (C 
  in 
  section) 
  Cam- 
  

  

  bric 
  (Conasarga 
  formation) 
  ; 
  piurr 
  -rq 
  Carboniferotis 
  (Floyd 
  

   shale). 
  Scale 
  T25W 
  

  

  ^ 
  

  

  anticlines, 
  it 
  must 
  be 
  inferred 
  that 
  the 
  folded 
  mass 
  has, 
  as 
  a 
  whole, 
  

   been 
  pushed 
  upon 
  the 
  first 
  series 
  to 
  an 
  unknown 
  extent. 
  Dr 
  

   Ulrich 
  with 
  whom 
  I 
  had 
  the 
  pleasure 
  of 
  discussing 
  this 
  view 
  dur- 
  

   ing- 
  our 
  summer 
  trips 
  into 
  

  

  c 
  ■ 
  — 
  • 
  : 
  — 
  the 
  Champlain 
  region, 
  

  

  reached 
  independently 
  a 
  

   like 
  view, 
  finding 
  positive 
  

   evidence 
  of 
  such 
  a 
  great 
  

   charriage 
  in 
  the 
  condi- 
  

   tions 
  surrounding 
  the 
  

   north 
  end 
  of 
  the 
  Taconic 
  mountains, 
  where 
  a 
  small 
  " 
  outlier 
  " 
  

   of 
  Stockbridge 
  limestone 
  appears 
  in 
  the 
  Cambric 
  rocks 
  and 
  belts 
  

   of 
  " 
  Hudson 
  slate 
  " 
  accompanying 
  the 
  Cambric 
  inlier 
  [see 
  text 
  

   ^-g- 
  33 
  1 
  on 
  the 
  west. 
  It 
  is 
  there 
  quite 
  probable 
  that 
  the- 
  whole 
  

  

  ^T 
  

  

  Fig. 
  32 
  Charriage 
  (after 
  Haug) 
  

  

  