﻿^ 
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  °l* 
  53'] 
  DEPOSITS 
  OF 
  THE 
  CLEEYE 
  HILL 
  PLATEAU. 
  

  

  609 
  

  

  close 
  to 
  the 
  1000-foot 
  contour-line. 
  The 
  other 
  beds 
  between 
  these 
  

   and 
  the 
  Harford 
  Sands 
  inclusive 
  (see 
  p. 
  615) 
  may 
  also 
  be 
  found 
  

   there. 
  

  

  It 
  is 
  now 
  advisable 
  to 
  go 
  to 
  Cleeve 
  Hill 
  itself, 
  and 
  of 
  the 
  

   numerous 
  exposures 
  to 
  be 
  seen 
  on 
  the 
  Common 
  to 
  give 
  the 
  fol- 
  

   lowing 
  generalized 
  section 
  of 
  results. 
  Afterwards 
  it 
  will 
  be 
  stated 
  

   where 
  the 
  different 
  beds 
  may 
  be 
  examined 
  to 
  the 
  best 
  advantage. 
  

  

  2. 
  Cleeve 
  Hill 
  ; 
  a 
  generalized 
  section. 
  

  

  Ft. 
  ins. 
  Ft. 
  ins. 
  

   Olypeus- 
  And 
  I. 
  1. 
  Yellow 
  ragstones 
  with 
  Terebratula 
  

   Upper 
  globata. 
  In 
  the 
  lower 
  part 
  are 
  

  

  Trigonia-grits. 
  numerous 
  Trigonice 
  and 
  Ehyncho- 
  

  

  netta 
  angulata 
  about 
  15 
  

  

  Terebratula 
  II. 
  1. 
  Bluish-grey, 
  sandy 
  stone, 
  sharp 
  

   Phillipsiana- 
  fracture. 
  Bored 
  by 
  annelids 
  and 
  

   beds. 
  Lithodomi 
  4 
  

  

  2. 
  Similar 
  stone, 
  not 
  bored, 
  but 
  some- 
  

  

  what 
  rounded 
  in 
  places, 
  and 
  with 
  

   sand-pockets 
  6 
  

  

  3. 
  Similar 
  deposit 
  ; 
  3 
  beds 
  with 
  sandy 
  

  

  partings. 
  Terebratula 
  Phillipsi- 
  

   ana, 
  var., 
  sparingly 
  [Upton] 
  5 
  

  

  4. 
  Similar 
  splintery 
  grey 
  limestone 
  

  

  with 
  Terebratula 
  Phillipsiana 
  

   and 
  T. 
  Buckmaniana 
  abundant. 
  

   ' 
  Ehynchonella 
  quadriplicata. 
  ' 
  

   Acanthothyris. 
  Two 
  beds 
  with 
  

   sandy 
  partings, 
  and 
  a 
  sandy 
  base 
  

   with 
  oysters 
  2 
  3 
  

  

  5. 
  Similar 
  massive 
  stone. 
  Terebratula 
  

  

  Phillipsiana, 
  ' 
  Rhynchonella 
  qua- 
  

   driplicata 
  ' 
  [Upton]. 
  Large 
  

   ' 
  Bourguetia 
  striata' 
  2 
  

  

  Bourguetia- 
  III. 
  1. 
  Greyish 
  shelly 
  stone 
  with 
  brownish 
  

   beds. 
  patches 
  and 
  infillings. 
  Ctenos- 
  

   treon 
  pectiniforme 
  or 
  proboscideum, 
  

   Bourguetia 
  1 
  2 
  3 
  

  

  2. 
  Grey 
  stone 
  in 
  several 
  beds. 
  La- 
  

  

  mellibranchiata 
  are 
  numerous 
  and 
  

   particularly 
  noticeable 
  for 
  their 
  

   unusually 
  large 
  size. 
  Large, 
  much- 
  

   plicate 
  Ostrea, 
  Myoconcha, 
  etc. 
  

   Large 
  Nautilus 
  7 
  

  

  3. 
  Grey 
  shelly 
  limestone, 
  somewhat 
  

  

  bored 
  1 
  6 
  

  

  4. 
  Limestone 
  9 
  

  

  5. 
  And 
  there 
  is 
  presumably 
  of 
  this 
  

  

  deposit 
  about 
  another 
  2 
  

  

  10 
  1 
  

  

  13 
  6 
  

  

  1 
  A 
  large, 
  umbilicate, 
  much-compressed, 
  crassicostate 
  Stephanoceras 
  was 
  

   found 
  by 
  Mr. 
  C. 
  Upton 
  2 
  feet 
  9 
  inches 
  below 
  the 
  Terebratula 
  Buckmaniana- 
  

   bed. 
  Its 
  matrix 
  and 
  position 
  indicate 
  this 
  bed 
  No. 
  1 
  . 
  

  

  Q. 
  J. 
  G. 
  S. 
  No. 
  212. 
  2 
  s 
  

  

  