﻿Vol. 
  53.] 
  THE 
  BAJOC1AN 
  OP 
  THE 
  CLEEYE 
  HILL 
  PLATEAU. 
  617 
  

  

  Table 
  vi., 
  published 
  with 
  the 
  Dundry 
  paper, 
  should 
  be 
  amended 
  in 
  

   accordance 
  with 
  this, 
  and 
  then 
  will 
  be 
  obtained 
  the 
  fullest 
  sequence 
  

   of 
  deposits 
  which 
  has 
  been 
  yet 
  noticed 
  in 
  the 
  Cotteswolds. 
  It 
  is 
  

   interesting 
  to 
  observe 
  that 
  the 
  Cotteswold 
  ' 
  Inferior 
  Oolite 
  ' 
  which 
  

   was 
  parted 
  into 
  three 
  divisions 
  by 
  Murchison 
  in 
  1834 
  * 
  is 
  now 
  

   divided 
  into 
  17 
  portions 
  of 
  varied 
  lithic 
  aspect, 
  with 
  particular 
  

   faunal 
  features. 
  Of 
  these 
  divisions, 
  14 
  lie 
  beneath 
  the 
  Upper 
  

   Trigonia-giit 
  ; 
  and 
  of 
  the 
  14, 
  different 
  localities 
  show 
  each 
  their 
  

   own 
  particular 
  number 
  to 
  be 
  present. 
  Thus, 
  in 
  a 
  south-to-north 
  

   traverse, 
  there 
  may 
  be 
  tabulated 
  as 
  present 
  beneath 
  the 
  Upper 
  

   Trigonia-grib 
  : 
  

  

  At 
  Uley 
  Bury, 
  Birdlip, 
  Leckhampton, 
  Cleeve 
  Hill, 
  

  

  2 
  5 
  10 
  14 
  divisions. 
  

  

  This 
  record 
  illustrates 
  the 
  difference 
  effected 
  mainly 
  by 
  denuda- 
  

   tion 
  prior 
  to 
  the 
  deposition 
  of 
  the 
  Upper 
  Trigonia-grit. 
  

  

  y. 
  cokkelation 
  op 
  the 
  cleeve 
  hlll 
  deposits 
  with 
  those 
  

   op 
  othek 
  Localities. 
  

  

  With 
  the 
  alterations 
  noted 
  above, 
  the 
  Cleeve 
  Hill 
  deposits 
  may 
  

   be 
  correlated 
  with 
  those 
  of 
  Dundry 
  and 
  Dorset-Somerset 
  according 
  

   to 
  the 
  table 
  given 
  in 
  the 
  paper 
  on 
  Dundry 
  Hill 
  just 
  quoted. 
  Only 
  

   those 
  slight 
  alterations 
  and 
  the 
  addition 
  of 
  the 
  Snowshill 
  Clay 
  are 
  

   required. 
  

  

  YI. 
  The 
  Strtjctuke 
  op 
  Part 
  op 
  Cleeve 
  Hill. 
  

  

  The 
  approximate 
  structure 
  of 
  the 
  upper 
  part 
  of 
  the 
  Cleeve 
  Hill 
  

   plateau, 
  from 
  the 
  top 
  of 
  Hewlett's 
  Hill 
  to 
  the 
  Rolling 
  Bank 
  quarry, 
  

   and 
  to 
  the 
  knoll 
  immediately 
  beyond 
  that, 
  is 
  illustrated 
  in 
  Diagr. 
  II. 
  2 
  

   Not 
  quite 
  a 
  straight 
  line 
  has 
  been 
  followed 
  — 
  or 
  rather 
  some 
  details 
  

   off 
  the 
  line 
  have 
  been 
  brought 
  into 
  the 
  general 
  line, 
  the 
  better 
  to 
  

   show 
  the 
  sequence 
  of 
  the 
  strata 
  and 
  their 
  position. 
  3 
  It 
  may 
  be 
  

   seen 
  that 
  there 
  are 
  seven 
  faults 
  noted 
  ; 
  three 
  of 
  these, 
  but 
  one 
  is 
  

   scarcely 
  worthy 
  of 
  the 
  name, 
  are 
  shown 
  in 
  the 
  Boiling 
  Bank 
  itself. 
  

   There 
  may 
  be 
  other 
  faults 
  hidden. 
  

  

  Of 
  these 
  faults, 
  No. 
  1, 
  near 
  Hewlett's 
  Hill, 
  is 
  shown 
  by 
  old 
  workings 
  

  

  1 
  ' 
  Geology 
  of 
  Cheltenham,' 
  p. 
  10. 
  

  

  2 
  A 
  note 
  may 
  be 
  made 
  concerning 
  what 
  I 
  have 
  called 
  the 
  Nerin&a-bed., 
  

   although 
  it 
  is 
  outside 
  the 
  scope 
  of 
  this 
  paper. 
  It 
  shows 
  some 
  fine 
  Nerincea, 
  

   and 
  it 
  also 
  yields 
  a 
  Terebratula 
  so 
  closely 
  like 
  T. 
  fimbria 
  that 
  it 
  would 
  be 
  called 
  

   that 
  fossil. 
  However, 
  certain 
  peculiar 
  characters 
  distinguish 
  it 
  from 
  the 
  

   Terebratula 
  fimbria 
  of 
  the 
  Oolite 
  Marl 
  — 
  it 
  is, 
  in 
  fact, 
  a 
  biologically 
  earlier 
  

   fossil, 
  and 
  is 
  the 
  parent 
  of 
  tbe 
  Oolite 
  Marl 
  shell. 
  The 
  bed 
  in 
  which 
  it 
  occurs 
  

   is 
  a 
  fossiliferous, 
  somewhat 
  pisolitic, 
  sandy 
  vein 
  in 
  the 
  Lower 
  Freestone. 
  I 
  am 
  

   not 
  at 
  present 
  able 
  to 
  say 
  how 
  far 
  the 
  bed 
  is 
  situated 
  below 
  the 
  Oolite 
  Marl, 
  or 
  

   above 
  the 
  Pea 
  Grit. 
  Possibly 
  it 
  has 
  been 
  hitherto 
  considered 
  as 
  Oolite 
  Marl. 
  

   The 
  interest 
  attaching 
  to 
  it 
  is 
  biological, 
  in 
  connexion 
  with 
  the 
  fimbriate 
  

  

  3 
  The 
  surface 
  of 
  the 
  ground, 
  with 
  the 
  approximate 
  height 
  shown, 
  is 
  such 
  as 
  

   would 
  be 
  found 
  by 
  any 
  one 
  making 
  a 
  traverse 
  along 
  the 
  hill-top 
  from 
  Hewlett's 
  

   to 
  beyond 
  the 
  Rolling 
  Bank. 
  

  

  