﻿532 
  Forty- 
  seventh 
  Report 
  on 
  the 
  State 
  Museum, 
  

  

  occupied 
  mainly 
  by 
  Hudson 
  river 
  shales 
  and 
  the 
  Clinton 
  members 
  

   but 
  in 
  which 
  there 
  are 
  no 
  outcrops. 
  

  

  About 
  Whiteport 
  station 
  and 
  northward, 
  the 
  Rosendale-White- 
  

   port 
  anticline 
  bears 
  upon 
  its 
  flanks 
  a 
  series 
  of 
  flexures 
  of 
  various 
  

   sizes, 
  the 
  relations 
  of 
  which 
  are 
  represented 
  in 
  the 
  following 
  figure. 
  

  

  Fig. 
  9.— 
  Cross-sections 
  of 
  region 
  about 
  Whiteport 
  station 
  and 
  the 
  Upper 
  Binnewaters. 
  

   Looking 
  north. 
  E., 
  Esopus 
  shales; 
  O., 
  Oriskany 
  sandstone; 
  US., 
  Upper 
  Shaly 
  limestone; 
  B., 
  

   Becraft 
  limestone; 
  LS., 
  Lower 
  Shaly 
  limestone; 
  P., 
  Pentamerus 
  limestone; 
  T., 
  Tentaculite 
  

   limestone; 
  C, 
  Cement 
  series; 
  CI., 
  Clinton 
  formation 
  ; 
  HR 
  M 
  Hudson 
  river 
  shales. 
  Vertical 
  scale 
  

   considerably 
  exaggerated. 
  

  

  It 
  may 
  be 
  seen 
  from 
  the 
  botton 
  section 
  in 
  this 
  figure 
  that 
  the 
  

   cement 
  beds 
  are 
  brought 
  near 
  to 
  the 
  surface 
  over 
  a 
  considerable 
  

  

  