﻿16 
  FEDDEN: 
  GEOLOGY 
  OF 
  kXtHIAwXr 
  PENINSULA 
  IN 
  GUZEEAT. 
  

  

  feet 
  echinoid 
  and 
  spines 
  were 
  obtained. 
  This 
  bed 
  is 
  tilted 
  at 
  about 
  

   80°, 
  to 
  south-30°-west. 
  The 
  sandstones 
  with 
  which 
  the 
  band 
  of 
  gritty 
  

   limestone 
  is 
  associated 
  are 
  also 
  turned 
  up 
  at 
  the 
  same 
  angle 
  just 
  at 
  this 
  

   spot. 
  There 
  is 
  no 
  clear 
  section, 
  and 
  the 
  rocks 
  are 
  confused. 
  

  

  At 
  Bhaduka 
  the 
  limestone 
  is 
  cherty, 
  with 
  small 
  segregations 
  running 
  

   in 
  the 
  direction 
  of 
  the 
  bedding 
  ; 
  it 
  is, 
  as 
  usual, 
  tilted 
  and 
  displaced. 
  

   There 
  is 
  here 
  a 
  still 
  greater 
  confusion 
  among 
  the 
  rocks 
  ; 
  traps 
  are 
  very 
  

   various, 
  including 
  volcanic 
  ash 
  and 
  agglomerate. 
  A 
  coarse 
  unlaminated 
  

   sandstone 
  — 
  evidently 
  a 
  rapid 
  accumulation, 
  as 
  from 
  floods 
  — 
  contains 
  

   rounded 
  masses 
  of 
  decomposed 
  amygdaloid, 
  and 
  portions 
  of 
  other 
  rock. 
  

  

  In 
  the 
  small 
  nala 
  on 
  the 
  south 
  side 
  of 
  the 
  high 
  road 
  east- 
  south-east 
  

   of 
  Bhaduka, 
  the 
  organic 
  limestone 
  is 
  seen 
  in 
  thick 
  masses 
  tilted 
  on 
  

   end. 
  The 
  rock 
  is 
  somewhat 
  silicious 
  and 
  very 
  tough. 
  It 
  was 
  from 
  

   this 
  locality 
  that 
  the 
  flattened 
  keeled 
  ammonite 
  was 
  obtained, 
  together 
  

   with 
  a 
  small 
  Ostrea 
  and 
  a 
  crenulated 
  Natica 
  {?), 
  besides 
  some 
  small 
  

   corals. 
  In 
  the 
  talaori 
  at 
  the 
  head 
  of 
  the 
  nala, 
  there 
  is 
  a 
  small 
  outcrop 
  

   of 
  the 
  limestone 
  apparently 
  dipping 
  5° 
  south 
  of 
  east 
  at 
  50° 
  — 
  60°, 
  but 
  no 
  

   other 
  rock 
  is 
  exposed 
  there. 
  

  

  Near 
  Sidsar, 
  a 
  village 
  three 
  miles 
  north 
  of 
  Sayla 
  (Sahila) 
  in 
  the 
  

   Wadhwan 
  district, 
  a 
  few 
  imperfect 
  fossils 
  (mostly 
  fragments 
  of 
  an 
  

   ostreoid 
  shell) 
  were 
  obtained 
  from 
  a 
  crumbling 
  calcareous 
  sandstone 
  

   associated 
  with 
  impure 
  limestone 
  and 
  various 
  other 
  thin 
  bands. 
  The 
  

   whole 
  extent 
  of 
  the 
  exposure 
  does 
  not 
  exceed 
  a 
  few 
  yards, 
  and 
  they 
  are 
  

   covered 
  up 
  by 
  traps 
  close 
  by. 
  

  

  Near 
  the 
  village 
  of 
  Ti*nba, 
  in 
  the 
  stream 
  that 
  passes 
  by 
  Kharwa, 
  

   south 
  of 
  Wadhwan- 
  city, 
  there 
  is 
  an 
  instance 
  of 
  abnormal 
  intercalation 
  of 
  

   sandy 
  beds 
  among 
  the 
  basal 
  trap 
  flows. 
  Trap 
  is 
  seen 
  both 
  above 
  and 
  

   below 
  these 
  at 
  this 
  point 
  of 
  the 
  section; 
  but 
  in 
  other 
  parts 
  of 
  the 
  

   section, 
  sedimentary 
  beds 
  are 
  tilted 
  at 
  high 
  angles, 
  and 
  the 
  conditions 
  

   appear 
  abnormal, 
  as 
  though 
  the 
  margin 
  of 
  the 
  latter 
  had 
  been 
  turned 
  

   up 
  and 
  imbedded 
  by 
  the 
  trap 
  flow. 
  

  

  Further 
  down 
  the 
  stream 
  there 
  is, 
  in 
  the 
  vicinity 
  of 
  Kharwa, 
  quite 
  

   a 
  jumble 
  of 
  various 
  and 
  heterogeneous 
  traps 
  with 
  sedimentary 
  accumu- 
  

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  ) 
  

  

  