﻿736 
  Forty-seventh 
  Report 
  on 
  the 
  State 
  Museum. 
  

  

  and 
  in 
  position 
  to 
  the 
  same 
  rock 
  as 
  elsewhere 
  noted. 
  Both 
  

   green 
  and 
  red 
  layers 
  are 
  highly 
  concretionary, 
  the 
  concretions 
  

   being 
  small, 
  irregular 
  and 
  confluent; 
  characteristic 
  examples 
  of 
  

   " 
  Kramenzel." 
  

  

  (5) 
  Gray 
  sandstones 
  presenting 
  thick 
  wall-faces, 
  but 
  coming 
  out 
  

   as 
  thin 
  flags. 
  Seven 
  feet. 
  

  

  (6) 
  Soft 
  red 
  shales. 
  Eight 
  feet. 
  

  

  (7) 
  Eed 
  flags 
  or 
  sandstones. 
  Two 
  feet 
  six 
  inches. 
  

  

  (8) 
  Soft 
  red 
  shales. 
  Three 
  feet. 
  

  

  JSTo 
  fossils, 
  except 
  as 
  already 
  specified, 
  were 
  observed 
  in 
  this 
  

   section. 
  

  

  Station 
  J. 
  Three 
  miles 
  northeast 
  of 
  Greene 
  and 
  one-half 
  mile 
  

   north 
  of 
  the 
  river 
  road 
  ; 
  quarry 
  on 
  the 
  property 
  of 
  Isaac 
  Edger- 
  

   ton. 
  At 
  base 
  : 
  

  

  3tat 
  

  

  IOTI 
  

  

  Scale 
  :- 
  

  

  m 
  

  

  sy 
  

  

  JLili 
  Li 
  JLilVLLt-ii-b3 
  : 
  P 
  g 
  i 
  s 
  r 
  f 
  

  

  •• 
  ■ 
  a 
  

  

  •J- 
  

   V- 
  — 
  - 
  

  

  (1) 
  Compact, 
  light 
  greenish 
  sandstone, 
  splitting 
  into 
  thin 
  flags 
  

   at 
  top, 
  but 
  thicker 
  at 
  the 
  bottom 
  ; 
  six 
  feet. 
  

  

  (2) 
  Brilliant 
  green 
  and 
  red, 
  soft 
  clay 
  shales 
  ; 
  one 
  foot. 
  

  

  (3) 
  Compact 
  red 
  sandstone, 
  schistose 
  on 
  exposure; 
  two 
  and 
  

   one-fourth 
  feet. 
  

  

  (4) 
  Eed 
  shales, 
  slightly 
  sandy 
  ; 
  two 
  and 
  one-fourth 
  feet. 
  

  

  (5) 
  Greenish 
  shaly 
  sandstone 
  with 
  " 
  f 
  ucoidal 
  " 
  surface 
  ; 
  toward 
  

   the 
  top 
  this 
  passes 
  into 
  greenish 
  and 
  reddish 
  shales 
  ; 
  two 
  feet. 
  

  

  (6) 
  Light 
  gray 
  sandstone 
  ; 
  one 
  foot, 
  six 
  inches. 
  

   ~No 
  fossils 
  were 
  observed 
  in 
  any 
  of 
  the 
  layers. 
  

  

  The 
  hill 
  roads 
  south 
  of 
  East 
  Greene 
  (Brisben) 
  afford 
  very 
  few 
  

   exposures 
  of 
  the 
  strata. 
  It 
  is, 
  however, 
  observable 
  that 
  the 
  

   upland 
  drift 
  and 
  high 
  level 
  gully- 
  wash 
  contains 
  a 
  very 
  considera- 
  

   ble 
  amount 
  of 
  blocks 
  containing 
  Chemung 
  fossils, 
  with, 
  fragments 
  

   of 
  red 
  sandstone. 
  

  

  /Section 
  K. 
  Greene 
  ; 
  on 
  property 
  of 
  J. 
  A. 
  Juliand, 
  east- 
  south- 
  

   east 
  of 
  village, 
  one-fourth 
  mile. 
  At 
  about 
  150 
  feet 
  above 
  the 
  

  

  