﻿Appalachian 
  Geosyncline. 
  

  

  455 
  

  

  Thick- 
  

   ness 
  

  

  Sum 
  

  

  Depth 
  

   helow 
  

   top 
  of 
  

   Pocono 
  

  

  Crossing 
  of 
  wagon 
  road 
  and 
  Lehigh 
  

   Valley 
  E. 
  E. 
  at 
  elevation 
  590 
  and 
  one-half 
  

   mile 
  N.N.W. 
  of 
  Conner's 
  Station 
  on 
  P. 
  & 
  

  

  E. 
  E. 
  E. 
  is 
  at 
  stratigraphic 
  level 
  —7310. 
  

  

  Red 
  shale 
  and 
  sandstone 
  140 
  560-7440 
  

  

  Catskill 
  — 
  Chemung 
  Transition 
  Beds. 
  

  

  Olive 
  shale 
  weathering 
  pale 
  yellow, 
  highest 
  

  

  Chemung 
  facies 
  but 
  probably 
  not 
  marine. 
  34 
  

  

  Olive 
  sandstone 
  12 
  

  

  Red 
  sandstone 
  6 
  

  

  Red 
  shale 
  23 
  

  

  Olive 
  shale 
  40 
  

  

  No 
  exposure 
  150 
  

  

  Red 
  sandstone 
  and 
  shale 
  interbedded. 
  Lowest 
  

   thick 
  red 
  beds 
  and 
  therefore 
  the 
  base 
  of 
  the 
  

  

  Catskill 
  70 
  335 
  -7775 
  

  

  Mud 
  cracks 
  and 
  rainprints 
  were 
  found 
  

   by 
  Dr. 
  A. 
  M. 
  Bateman 
  and 
  the 
  writer 
  in 
  

   1912 
  four 
  and 
  a 
  half 
  miles 
  southeast 
  by 
  east 
  

   of 
  this 
  point 
  at 
  Landingville 
  in 
  the 
  basal 
  

   red 
  shale 
  exposed 
  in 
  that 
  section. 
  

  

  Chemung 
  Formation, 
  passing 
  below 
  into 
  the 
  Senecan 
  

   (Portage) 
  Group. 
  Gray 
  and 
  olive 
  sandy 
  

   shales 
  in 
  upper 
  portion, 
  but 
  the 
  base 
  of 
  this 
  

   member 
  need 
  not 
  correspond 
  with 
  base 
  of 
  

   Neiv 
  York 
  Chemung. 
  

  

  Yellowish 
  gray 
  shale 
  59 
  

  

  Red 
  shale 
  _ 
  1 
  

  

  Pale 
  red 
  sandstone 
  _ 
  10 
  —7845 
  

  

  Yellowish 
  sandstone 
  in 
  soft 
  olive 
  shales 
  . 
  _ 
  15 
  

  

  Soft 
  bluish 
  gray 
  shales 
  70 
  

  

  Not 
  exposed, 
  mostly 
  soft 
  gray 
  shales 
  293 
  

  

  Sandy 
  gray 
  and 
  olive 
  shales 
  and 
  some 
  sandstones 
  

   with 
  marine 
  fossils, 
  collected 
  from 
  surface 
  

   rock 
  about 
  —8250 
  to 
  —8450. 
  Section 
  not 
  

   exposed. 
  

  

  F. 
  Crinoid 
  ossicles 
  and 
  columns. 
  Spirifer 
  

  

  mesastrialis 
  t 
  ._ 
  235 
  683-8458 
  

  

  Flaggy 
  sandstones 
  interbedded 
  with 
  dark 
  

   siliceous 
  shales. 
  

   Dark 
  gray 
  shales 
  and 
  flaggy 
  sandstones, 
  not 
  well 
  

  

  exposed 
  132 
  

  

  A 
  probable 
  error 
  introduced 
  here 
  of 
  25 
  

   or 
  50 
  feet 
  and 
  affecting 
  the 
  stratigraphic 
  

   level 
  of 
  the 
  beds 
  below. 
  Strata 
  affected 
  by 
  

   a 
  local 
  fold 
  below 
  this 
  member 
  and 
  one 
  

   omission 
  made 
  in 
  measurement. 
  

   E. 
  An 
  abundance 
  of 
  crinoid 
  stems 
  and 
  

  

  two 
  species 
  of 
  pelecypods 
  —8590 
  

  

  Dark 
  gray 
  shales 
  and 
  flaggy 
  sandstones 
  65 
  —8655 
  

  

  Red 
  shale 
  and 
  brown 
  sandstone. 
  The 
  lowest 
  

  

  red 
  shale 
  . 
  25 
  —8680 
  

  

  Thick 
  bedded 
  olive 
  sandstones 
  with 
  thin 
  bedded 
  

   olive 
  shales. 
  Some 
  conglomeratic 
  beds 
  

   holding 
  pebbles 
  of 
  white 
  quartz 
  up 
  to 
  0*5 
  

   in. 
  in 
  diameter. 
  Some 
  coarse 
  plant 
  im- 
  

   pressions 
  100 
  -8780 
  

  

  