﻿THE 
  GEOLOGICAL 
  HISTORY 
  OF 
  NEW 
  YORK 
  STATE 
  

  

  53 
  

  

  sider 
  that 
  sedimentation 
  was 
  uninterrupted, 
  though 
  as 
  a 
  matter 
  of 
  

   fact 
  there 
  were 
  certainly 
  minor 
  oscillations 
  of 
  level 
  which 
  inter- 
  

  

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  •Sea. 
  level 
  

  

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  Sea 
  (eveT 
  

  

  i 
  I 
  frpnkfor+(Onfo- 
  v 
  , 
  e 
  „ 
  3 
  Onei'c/a(Si/urt'c) 
  \VTTTT\C//hfor?f5//.) 
  ] 
  sha/er. 
  

  

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  ~J 
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  sho/es 
  \ 
  o°£2°A 
  Cony/omer&fe 
  III 
  II 
  W 
  sone/sforKf/rvwd' 
  

  

  I 
  anc/ 
  times 
  forte 
  

  

  ilou/er 
  So/ina.or 
  W///X 
  (/ppe/-Sff//hafS/Vfrc\^Q^hM,/f'cy?abi4f 
  ^aay 
  y\tre/c/er6em(Dei/o- 
  

  

  vucrterf/mes 
  ' 
  

  

  Fig. 
  17 
  Geologic 
  and 
  topographic 
  map 
  and 
  structure 
  sections 
  of 
  the 
  vicin- 
  

   ity 
  of 
  Clinton 
  (Oneida 
  county) 
  showing 
  the 
  surface 
  distribution 
  and 
  under- 
  

   ground 
  relations 
  of 
  the 
  various 
  rock 
  formations 
  from 
  the 
  Upper 
  Ordovicic 
  

   to 
  the 
  Lower 
  Devonic 
  inclusive. 
  Note 
  the 
  simple 
  nonfolded 
  and 
  nonfaulted 
  

   structure, 
  and 
  the 
  gentle 
  southwesterly 
  dip 
  (tilt) 
  of 
  the 
  formations. 
  A 
  simi- 
  

   lar 
  simple 
  structure 
  characterizes 
  the 
  formations 
  of 
  the 
  whole 
  southwestern 
  

   plateau 
  province. 
  Vertical 
  scale 
  of 
  the 
  sections 
  four 
  times 
  exaggerated. 
  

  

  Geology 
  by 
  W. 
  J. 
  Miller 
  

  

  fered 
  with 
  the 
  deposition 
  of 
  sediments 
  and 
  produced 
  slight 
  uncon- 
  

   formities. 
  These 
  minor 
  interruptions 
  have 
  not 
  yet 
  been 
  carefully 
  

  

  