﻿666 
  FORTY-SEVENTH 
  REPORT 
  ON 
  TEE 
  STATE 
  MUSEUM. 
  

  

  Series 
  II. 
  No 
  evidence 
  of 
  the 
  crystalline 
  limestones 
  has 
  been 
  

   noted. 
  

  

  Series 
  III. 
  Undoubtedly 
  much 
  of 
  the 
  eastern 
  portion 
  con- 
  

   sists 
  of 
  this 
  rock. 
  It 
  will 
  be 
  investigated 
  another 
  season. 
  I 
  was 
  

   obliged 
  to 
  return 
  October 
  1st, 
  without 
  investigating 
  it. 
  

  

  Series 
  IV. 
  No 
  palaeozoic 
  rocks 
  are 
  present. 
  

  

  Series 
  V. 
  No 
  dikes 
  have 
  thus 
  far 
  been 
  seen. 
  

  

  Series 
  VI. 
  The 
  Pleistocene 
  sands 
  and 
  gravels 
  are 
  well 
  shown, 
  

   but 
  reach 
  their 
  greatest 
  development 
  near 
  Bloomingdale 
  and 
  

   further 
  west 
  and 
  north. 
  Bloomiogdale 
  station, 
  on 
  the 
  Chateau- 
  

   gay 
  railroad, 
  is 
  outside 
  the 
  township, 
  but 
  is 
  built 
  on 
  a 
  superb 
  lake 
  

   bottom, 
  over 
  which 
  the 
  track 
  is 
  laid 
  for 
  several 
  miles 
  almost 
  on 
  

   a 
  dead 
  level. 
  In 
  other 
  respects 
  no 
  developments 
  of 
  special 
  

   interest 
  were 
  met. 
  

  

  Yours 
  respectfully, 
  

  

  J. 
  F. 
  KEMP. 
  

  

  