﻿180 
  ON 
  GLACIAL 
  TKACES 
  IN 
  THE 
  LAKE-LISTKICT 
  AND 
  NOKTH 
  WALES. 
  

  

  Prof. 
  Eamsay 
  observed 
  that 
  some 
  years 
  ago 
  he 
  had 
  attempted 
  to 
  

   show 
  that 
  Anglesea 
  had 
  been 
  glaciated 
  by 
  ice 
  that 
  had 
  come 
  from 
  

   the 
  north 
  in 
  the 
  Cumberland 
  district, 
  and 
  attributed 
  this 
  circum- 
  

   stance 
  to 
  the 
  preponderance 
  of 
  this 
  northern 
  ice 
  over 
  that 
  from 
  the 
  

   Snowdon 
  range, 
  which 
  was, 
  as 
  it 
  were, 
  set 
  aside 
  by 
  it. 
  He 
  was 
  

   inclined 
  to 
  think 
  that 
  the 
  Menai 
  Straits, 
  the 
  direction 
  of 
  which 
  

   coincided 
  with 
  the 
  main 
  lines 
  of 
  glaciation 
  in 
  Anglesea, 
  might 
  be 
  

   due 
  to 
  the 
  same 
  cause. 
  

  

  