﻿74 
  A. 
  B. 
  WYNNE 
  ON 
  SOME 
  FEATURES 
  IN 
  THE 
  

  

  it 
  should 
  be 
  remembered 
  that 
  the 
  depth 
  of 
  this 
  bay 
  is 
  twenty 
  miles 
  

   on 
  its 
  shortest 
  side, 
  lying 
  within 
  British 
  territory, 
  on 
  the 
  right 
  

   bank 
  of 
  the 
  Jhilam, 
  that 
  this 
  side 
  is 
  there 
  nearly 
  a 
  straight 
  line, 
  and 
  

   as 
  strongly 
  resembles 
  a 
  fault 
  separating 
  highly 
  contorted 
  rocks 
  as 
  any 
  

   other 
  portion 
  of 
  the 
  contact. 
  Examined 
  in 
  the 
  same 
  way, 
  other 
  parts 
  

   of 
  the 
  junction 
  lose 
  much 
  of 
  their 
  apparent 
  sinuosity. 
  

  

  17. 
  The 
  sudden 
  change 
  in 
  the 
  direction 
  of 
  the 
  ranges 
  and 
  strike 
  of 
  

   the 
  rocks 
  in 
  the 
  Jhilam 
  valley 
  has 
  been 
  already 
  mentioned 
  ; 
  and 
  in 
  this 
  

   connexion 
  it 
  is 
  somewhat 
  singular 
  to 
  mark 
  that 
  on 
  the 
  further 
  side 
  

   of 
  that 
  river 
  from 
  our 
  district, 
  in 
  the 
  tributary 
  valley 
  of 
  the 
  Poonch 
  

   (Kashmere), 
  occurs 
  the 
  nearest 
  instance 
  of 
  the 
  unconformity 
  con- 
  

   tended 
  for 
  by 
  Mr. 
  Medlicott, 
  at 
  a 
  place 
  called 
  Dundelee. 
  The 
  strike 
  

   of 
  the 
  rocks 
  (E. 
  35° 
  S.) 
  belongs 
  to 
  the 
  same 
  system 
  as 
  that 
  of 
  the 
  

   Himalaya 
  east 
  of 
  the 
  Jhilam 
  valley 
  ; 
  and 
  the 
  section 
  as 
  given 
  in 
  Mr. 
  

   Medlicott's 
  report 
  is 
  extracted 
  (fig. 
  5) 
  for 
  comparison 
  with 
  those 
  

  

  Fig. 
  5. 
  — 
  Section 
  at 
  Dundelee, 
  Poonch 
  Valley. 
  

   (From 
  'Mem. 
  Greol. 
  Surv. 
  India,' 
  vol. 
  iii. 
  pi. 
  2, 
  p. 
  96.) 
  

  

  c\ 
  Krql 
  group, 
  c 
  2 
  . 
  Infra-Krol. 
  d. 
  Subathu 
  group. 
  

  

  within 
  our 
  district 
  (figs. 
  2, 
  3, 
  and 
  4) 
  and 
  lying 
  about 
  45 
  miles 
  to 
  the 
  

   west-north-west. 
  

  

  The 
  " 
  hard 
  blue 
  limestone," 
  c 
  1 
  , 
  in 
  this 
  section, 
  taken 
  by 
  Mr. 
  Med- 
  

   licott 
  to 
  represent 
  his 
  Krol 
  subdivision, 
  if 
  it 
  is 
  the 
  same 
  as 
  that 
  of 
  

   Mochipoora 
  Mountain 
  (as 
  may 
  be 
  gathered 
  from 
  a 
  footnote 
  at 
  p. 
  92 
  

   of 
  the 
  Report), 
  is 
  most 
  probably 
  Nummulitic, 
  or 
  might 
  also 
  include 
  

   some 
  of 
  the 
  Triassic 
  limestones 
  of 
  that 
  range 
  ; 
  at 
  any 
  rate 
  it 
  would 
  

   appear 
  to 
  belong 
  to 
  the 
  Hill-limestone 
  rocks, 
  c 
  2 
  is 
  said 
  to 
  be 
  com- 
  

   posed 
  of 
  " 
  thin 
  carbonaceous 
  slaty 
  shales," 
  which, 
  if 
  they 
  are 
  the 
  same 
  

   as 
  those 
  of 
  Shah-durrah, 
  mentioned 
  in 
  the 
  succeeding 
  passage, 
  pro- 
  

   bably 
  belong 
  to 
  the 
  zone 
  marked 
  d? 
  in 
  the 
  section 
  fig. 
  5 
  ; 
  indeed 
  

   this 
  might 
  be 
  inferred 
  from 
  the 
  parallelism 
  to 
  the 
  latter 
  which 
  

   Mr. 
  Medlicott 
  mentions, 
  d 
  2 
  , 
  red 
  sandstone 
  and 
  clays, 
  and 
  d 
  3 
  , 
  num- 
  

   mulitic 
  clays 
  (and 
  limestones 
  ?), 
  are 
  evidently 
  the 
  same 
  as 
  those 
  of 
  

   the 
  Murree 
  beds 
  previously 
  described 
  under 
  letter 
  E. 
  If 
  the 
  slaty 
  

   shales 
  c 
  2 
  pass 
  conformably 
  below 
  .the 
  limestone 
  c 
  1 
  , 
  they 
  probably 
  

   represent 
  some 
  of 
  the 
  many 
  hard 
  splintery 
  shaly 
  beds 
  of 
  the 
  Mochi- 
  

   poora 
  nummulitic 
  rocks. 
  

  

  Of 
  course, 
  without 
  having 
  seen 
  the 
  Dundelee 
  section, 
  these 
  remarks 
  

   upon 
  it 
  are 
  given 
  with 
  reserve 
  ; 
  still 
  it 
  is 
  much 
  nearer 
  to 
  our 
  district 
  

   than 
  to 
  the 
  Simla 
  area, 
  and 
  this 
  must 
  be 
  the 
  excuse 
  for 
  an 
  attempt 
  

   to 
  interpret 
  it 
  according 
  to 
  Upper-Punjab 
  experience. 
  

  

  