﻿Report 
  of 
  tee 
  State 
  Geologist. 
  

  

  733 
  

  

  usually 
  stained 
  with 
  bright 
  red 
  and 
  green 
  tints. 
  The 
  concre- 
  

   tionary 
  goniatite 
  layer 
  of 
  Ontario 
  county 
  unquestionably 
  repre- 
  

   sents 
  a 
  brief 
  repetition 
  of 
  the 
  physical 
  conditions 
  under 
  which 
  

   the 
  same 
  fauna 
  existed 
  in 
  Germany. 
  Similarly, 
  the 
  "Kramenzel" 
  

   of 
  station 
  D 
  must 
  also 
  represent 
  like 
  physical 
  conditions, 
  though 
  

   barren 
  of 
  organic 
  remains, 
  and 
  the 
  agreement 
  is 
  all 
  the 
  more 
  

   remarkable, 
  as 
  only 
  in 
  upper 
  Devonian 
  horizons 
  has 
  this 
  highly- 
  

   colored 
  "Kramenzel" 
  been 
  observed. 
  

  

  In 
  the 
  accompanying 
  sketch 
  is 
  a 
  restoration 
  of 
  the 
  geological 
  

   succession 
  from 
  station 
  A 
  to 
  E, 
  that 
  is, 
  from 
  near 
  the 
  level 
  of 
  

   the 
  Chenango 
  river 
  to 
  the 
  summit 
  of 
  the 
  high 
  watershed 
  on 
  the 
  

   west. 
  

  

  Station 
  F. 
  The 
  F. 
  G. 
  Clark 
  Company 
  quarry, 
  Oxford. 
  

  

  The 
  section 
  here 
  is 
  approximately 
  as 
  follows 
  ; 
  at 
  base]: 
  

  

  Station 
  F. 
  

  

  Scale:- 
  

  

  (1) 
  compact, 
  very 
  slightly 
  schistose, 
  even-grained, 
  greenish-gray 
  

   to 
  bluish 
  sandstone 
  with 
  obscure 
  lamination. 
  This 
  basal 
  layer 
  is 
  

   the 
  one 
  worked, 
  all 
  the 
  section 
  overlying 
  being 
  stripped. 
  Twenty- 
  

   five 
  feet. 
  

  

  (2) 
  Irregularly 
  jointed, 
  somewhat 
  shaly 
  sandstone, 
  of 
  greenish 
  

   tints 
  changing 
  to 
  red 
  toward 
  the 
  top. 
  Ten 
  feet. 
  Mr. 
  Edward 
  

   E 
  . 
  Davis, 
  of 
  Norwich, 
  N. 
  Y., 
  has 
  recently 
  informed 
  me 
  that 
  he 
  

   has 
  found 
  specimens 
  of 
  Amnigenia 
  Gatshillensis 
  in 
  this 
  layer 
  

   just 
  above 
  the 
  heavy-bedded 
  sandstone. 
  

  

  (3) 
  Green 
  and 
  red 
  compact 
  sandstones, 
  highly 
  concretionary 
  

   (compare 
  Station 
  D-3). 
  The 
  red 
  soft 
  shales 
  in 
  this 
  mass 
  which 
  

  

  