﻿THE 
  LAKE-DISTRICT 
  AND 
  NORTH 
  WALES. 
  175 
  

  

  Primary 
  glaciation. 
  

  

  Loughrigg 
  Tarn 
  and 
  the 
  neighbourhood, 
  striae 
  from 
  

  

  about 
  N.N.W. 
  and 
  N. 
  by 
  W. 
  

  

  In 
  one 
  place 
  crossed 
  by 
  striae 
  from 
  about 
  N.W. 
  

  

  North 
  side 
  of 
  Brathay 
  valley 
  (between 
  Loughrigg 
  Tarn 
  

  

  and 
  Clappersgate), 
  stria; 
  from 
  N.W. 
  

  

  Crossed 
  by 
  striae 
  from 
  a 
  little 
  N. 
  of 
  W. 
  

  

  Near 
  Pull 
  (on 
  road 
  from 
  Clappersgate 
  to 
  Hawkstead), 
  

  

  striae 
  from 
  about 
  N. 
  27° 
  W. 
  

  

  Quarry 
  near 
  Mr. 
  Atkinson's 
  house 
  (north-west 
  of 
  Win- 
  

   dermere), 
  striae 
  from 
  N. 
  30° 
  W. 
  

  

  Crossed 
  by 
  later 
  striae 
  from 
  N. 
  10° 
  W. 
  

  

  Windermere 
  churchyard, 
  broad 
  grooves 
  from 
  N. 
  25° 
  W. 
  

  

  Crossed 
  by 
  sharp 
  striae 
  from 
  N. 
  10° 
  W. 
  

  

  Near 
  Mr. 
  Pritt's 
  house, 
  Bowness, 
  striae 
  from 
  N. 
  30° 
  W. 
  

  

  In 
  front 
  of 
  a 
  house 
  called 
  the 
  Perns, 
  Windermere, 
  striae 
  

  

  from 
  between 
  N. 
  20° 
  and 
  N. 
  30° 
  W. 
  

  

  Near 
  Rev. 
  Mr. 
  Stock's 
  house, 
  Bowness, 
  striae 
  (possibly 
  

  

  secondary) 
  from 
  N. 
  10° 
  W. 
  

  

  Near 
  Crossings 
  (Windermere) 
  broad 
  grooves, 
  from 
  

  

  between 
  N. 
  20° 
  and 
  23° 
  W. 
  

  

  Crossed 
  by 
  striae 
  from 
  about 
  W. 
  35° 
  N., 
  and 
  a 
  few 
  

   grooves 
  from 
  about 
  N. 
  33° 
  W. 
  

  

  About 
  halfway 
  between 
  Windermere 
  and 
  the 
  Lake, 
  

  

  striae 
  from 
  N. 
  33° 
  W. 
  

  

  Orrest 
  Head 
  (Windermere), 
  smoothed 
  from 
  about 
  N.N.W. 
  

  

  Top 
  of 
  a 
  high 
  ridge 
  called 
  School 
  Knott 
  (near 
  Winder- 
  

   mere), 
  crossed 
  by 
  great 
  grooves 
  from 
  N. 
  33° 
  W. 
  

  

  Near 
  Ings 
  (east 
  of 
  Windermere) 
  a 
  number 
  of 
  large 
  

  

  roches 
  moutonnees 
  smoothed 
  from 
  about 
  N.N.W. 
  

  

  Broad 
  grooves 
  and 
  striae 
  on 
  ditto, 
  from 
  between 
  N. 
  20° 
  and 
  30° 
  W. 
  

  

  Bocks 
  at 
  a 
  considerable 
  height 
  on 
  west 
  side 
  of 
  Trout- 
  

   beck 
  valley, 
  smoothed 
  from 
  about 
  N.N.W. 
  

  

  Watershed 
  between 
  Style 
  End 
  (Kentmere) 
  and 
  Long 
  

   Sleddale, 
  striae 
  from 
  N. 
  

  

  West 
  of 
  Stavely 
  Parsonage, 
  primary 
  glaciation 
  from 
  

  

  about 
  N.W. 
  

  

  Crossed 
  by 
  large 
  grooves 
  from 
  nearly 
  W. 
  

  

  Near 
  entrance 
  to 
  Tilberthwaite 
  valley 
  (about 
  High 
  

   Yewdale, 
  Coniston), 
  rocks 
  extensively 
  smoothed 
  up 
  hill 
  

   from 
  about 
  N. 
  

  

  North 
  side 
  of 
  Church 
  Beck 
  valley 
  about 
  halfway 
  between 
  

   Coniston 
  and 
  Copper-works, 
  rocks 
  extensively 
  grooved 
  

  

  obliquely 
  down 
  hill 
  from 
  about 
  N. 
  

  

  Crossed 
  by 
  striae 
  running 
  in 
  direction 
  of 
  valley 
  or 
  

   from 
  N.N.W. 
  

  

  Near 
  Copper-works, 
  striae 
  (covered 
  with 
  stratified 
  sand 
  

  

  and 
  gravel) 
  from 
  N.N.W. 
  

  

  Between 
  Copper-works 
  and 
  Paddy 
  End, 
  striae 
  from 
  N. 
  30° 
  W. 
  

  

  At 
  mouth 
  of 
  Reddale 
  valley 
  above 
  Copper-works, 
  striae 
  

  

  from 
  N.W. 
  

  

  On 
  steep 
  slope 
  above 
  Copper-works, 
  rocks 
  extensively 
  

  

  striated 
  down 
  hill 
  from 
  about 
  N. 
  10° 
  W. 
  

  

  Roches 
  moutonnees 
  on 
  nearly 
  opposite 
  slope, 
  smoothed 
  

   up 
  hill 
  from 
  about 
  N. 
  

  

  Between 
  Duddon 
  Bridge 
  and 
  Seathwaite 
  Church, 
  roches 
  

   moutonnees 
  with 
  parallel 
  undulations 
  and 
  striae 
  coin- 
  

   ciding 
  in 
  direction, 
  from 
  about 
  N.N.E. 
  

  

  It 
  will 
  be 
  seen 
  from 
  the 
  above 
  statement 
  of 
  facts 
  that 
  the 
  pri- 
  

   mary 
  ice-marks 
  embrace 
  an 
  area 
  extending 
  from 
  near 
  Style 
  End 
  

  

  o2 
  

  

  