﻿I«2 
  

  

  NEW 
  YORK 
  STATE 
  MUSEUM 
  

  

  Smaller 
  anticline 
  inliers 
  may 
  sometimes 
  be 
  also 
  observed 
  in 
  the 
  

   plateau 
  regions 
  of 
  the 
  central 
  part 
  of 
  the 
  State 
  where 
  a 
  series 
  of 
  

   gentle 
  folds 
  representing 
  further 
  extension 
  of 
  the 
  Appalachian 
  

   mountain 
  folding 
  have 
  been 
  traced 
  by 
  Kindle.^ 
  Occasionally 
  a 
  

   small 
  inlier 
  wih 
  even 
  bring 
  out 
  the 
  presence 
  of 
  a 
  fold 
  in. 
  a 
  region 
  

   where 
  there 
  seem 
  to 
  be 
  no 
  indications 
  of 
  folding 
  at 
  all. 
  Thus 
  the 
  

   writer 
  observed 
  a 
  small 
  Lowville 
  limestone 
  inlier 
  coming 
  up 
  from 
  

   Lake 
  Ontario 
  at 
  Three 
  Mile 
  bay 
  (Clayton 
  quadrangle, 
  N. 
  Y.). 
  

  

  This 
  [see 
  text 
  fig. 
  9, 
  inlier 
  i] 
  

   follows 
  first 
  the 
  brook, 
  but 
  

   about 
  34 
  of 
  a 
  mile 
  above 
  its 
  

   mouth, 
  it 
  leaves 
  the 
  brook 
  

   and 
  rises 
  upon 
  the 
  hillside, 
  

   ending 
  just 
  east 
  of- 
  the 
  Three 
  

   Mile 
  Bay 
  railroad 
  station. 
  

   Here, 
  in 
  a 
  quarry, 
  the 
  arch 
  

   of 
  the 
  fold 
  is 
  exposed 
  in 
  the 
  

   Lowville 
  limestone 
  beds, 
  with 
  

   the 
  Black 
  River 
  on 
  the 
  flanks. 
  

   In 
  the 
  arid 
  regions 
  of 
  the 
  

   A'Vest, 
  where 
  neither 
  drift 
  nor 
  

   alluvial 
  deposits 
  obscure 
  the 
  

   outlines 
  of 
  inliers, 
  the 
  inti- 
  

   mate 
  relations 
  of 
  inliers 
  and 
  

  

  Fig. 
  22 
  Inlier 
  on 
  ciest 
  of 
  arch 
  oa 
  Pueblo 
  folds 
  are 
  mUch 
  clcarCr 
  shoWU 
  

  

  folio, 
  Col 
  

  

  stone. 
  

  

  Carlisle 
  shale 
  and 
  sand- 
  

  

  and 
  forms 
  of 
  bizarre 
  outline 
  

   produced 
  by 
  atmospheric 
  

   weathering. 
  We 
  insert, 
  as 
  

   an 
  example 
  [see 
  text 
  fig. 
  22, 
  

   23] 
  taken 
  almost 
  at 
  random, 
  a 
  sketch 
  from 
  the 
  Pueblo 
  folio. 
  Col. 
  

  

  Niobrara 
  shale. 
  

   Niobrara 
  limestone. 
  Scale 
  xssWtj 
  

  

  

  Fig. 
  23 
  Cress 
  section 
  of 
  arch 
  showirg 
  formation 
  of 
  inlier. 
  Pueblo 
  folio, 
  Col. 
  

  

  ^ 
  Kindle, 
  E. 
  M. 
  Jour. 
  Geol. 
  1904. 
  v. 
  XII, 
  no. 
  4, 
  p. 
  :?8i. 
  See 
  also 
  Luther, 
  

   D. 
  D. 
  N. 
  Y. 
  State 
  Mus. 
  Bui. 
  128. 
  Colored 
  section. 
  

  

  