﻿PHYSICAL 
  GEOLOGY 
  OF 
  THE 
  UPPER 
  PUNJAB. 
  

  

  73 
  

  

  the 
  same 
  orographical 
  position. 
  Even 
  in 
  the 
  Simla 
  area 
  a 
  fault-like 
  

   character 
  is 
  attributed 
  to 
  the 
  abnormal 
  junction 
  ; 
  and 
  had 
  we 
  here 
  

   the 
  transgressive 
  overlap 
  of 
  different 
  portions 
  of 
  the 
  Tertiary 
  series 
  

   on 
  to 
  the 
  hill-rocks, 
  it 
  might 
  be 
  easier 
  to 
  assimilate 
  the 
  features 
  of 
  

   the 
  two 
  areas 
  and 
  to 
  admit 
  for 
  this 
  district 
  Mr. 
  Medlicott's 
  view 
  

   that 
  the 
  junction-line 
  is 
  not 
  one 
  of 
  fault 
  but 
  of 
  unconformity. 
  

  

  

  (50 
  S 
  

  

  3 
  | 
  

  

  

  <D 
  ID 
  

  

  a 
  a 
  

  

  81 
  

  

  § 
  9 
  

   °i3 
  

  

  h- 
  a 
  

  

  r 
  O 
  i 
  

  

  ^2 
  

  

  ■II 
  

  

  a^ 
  

  

  s 
  

  

  Placing 
  the 
  more 
  northern 
  contact-lines 
  as 
  indicated 
  in 
  the 
  fore- 
  

   going 
  observations, 
  and 
  those 
  of 
  the 
  Simla 
  area 
  also, 
  upon 
  a 
  map 
  of 
  

   small 
  scale, 
  they 
  seem, 
  thus 
  reduced, 
  to 
  possess 
  considerable 
  irregu- 
  

   larity, 
  favouring 
  the 
  idea 
  of 
  unconformity, 
  as 
  in 
  the 
  case 
  of 
  the 
  deep 
  

   sinus 
  coinciding 
  with 
  the 
  bend 
  of 
  the 
  Jhilam 
  at 
  Mozufferabad 
  ; 
  but 
  

  

  