﻿236 
  Lahee 
  — 
  New 
  Fossiliferous 
  Horizon 
  and 
  Underlying 
  

  

  recognized 
  ; 
  but 
  they 
  are 
  nearly 
  always 
  much 
  decomposed. 
  

   Epidote 
  and 
  sericite, 
  disseminated 
  through 
  the 
  decaying 
  min- 
  

   erals, 
  are 
  most 
  abundant 
  as 
  alteration 
  products. 
  A 
  little 
  calcite, 
  

  

  l*<( 
  

  

  

  

  

  £ 
  

  

  

  

  

  

  \ 
  

  

  1% 
  

  

  t^ 
  * 
  

  

  

  s 
  

  

  ^ 
  

  

  vO 
  1 
  

  

  i%<r^ 
  

  

  

  Yy 
  + 
  < 
  

  

  l 
  + 
  + 
  + 
  + 
  

  

  >.*+♦ 
  

  

  

  r 
  +V 
  

  

  

  + 
  '♦■"♦' 
  

  

  

  I***-' 
  

  

  

  + 
  + 
  ^ 
  - 
  

  

  

  + 
  +■ 
  _ 
  

  

  n 
  

  

  

  

  .^ 
  ;; 
  

  

  

  f 
  +** 
  

  

  

  + 
  + 
  ++ 
  

  

  

  + 
  + 
  + 
  + 
  

  

  

  

  

  ++ 
  + 
  * 
  

  

  

  »-+ 
  + 
  + 
  

  

  

  

  

  

  

  4- 
  ■»- 
  + 
  + 
  

  

  

  >. 
  + 
  + 
  

  

  

  ■*■+ 
  + 
  + 
  

  

  

  K++ 
  + 
  

  

  

  fev 
  

  

  

  #+v 
  

  

  

  

  

  +"■**■ 
  + 
  

  

  

  ****v^ 
  

  

  

  

  

  

  

  

  

  

  

  ;****» 
  

  

  

  

  

  Sh 
  

  

  

  SSs 
  

  

  

  Ht5|| 
  

  

  si 
  

  

  

  is 
  

  

  'gtfg 
  

  

  lilillll 
  

  

  Q 
  

  

  

  

  bo 
  

  

  

  

  <G 
  

  

  £* 
  : 
  ^ 
  

  

  

  " 
  — 
  ' 
  

  

  P 
  ^ 
  

   *?|| 
  

  

  

  s 
  

  

  o 
  

  

  -*3 
  

  

  

  

  

  efl 
  

  

  

  

  

  o 
  

  

  

  

  

  

  

  

  

  T3 
  

  

  

  j£. 
  

  

  

  d 
  

  

  

  

  

  

  

  

  

  

  CO 
  

  

  

  

  <© 
  

  

  

  

  

  u 
  

  

  

  =g 
  

  

  

  cC 
  

  

  

  g| 
  

  

  

  rd 
  

  

  *»pk 
  

  

  

  o 
  

  

  ryl 
  

  

  

  1 
  

  

  o 
  

   to 
  

   o 
  . 
  

  

  _, 
  & 
  

  

  

  

  

  

  £ 
  "+ 
  3 
  

  

  

  

  03 
  

  

  

  

  OS 
  

  

  

  

  O* 
  

  

  

  

  I 
  ® 
  

  

  

  

  o 
  S 
  

  

  

  

  ~ 
  as 
  

  

  

  

  m 
  "° 
  

  

  

  ffcfSl- 
  

  

  

  

  "^liil 
  

  

  *J 
  

  

  

  *ov^ 
  

  

  ^.2 
  

  

  

  *■* 
  fpi 
  

  

  

  

  

  9 
  » 
  

  

  «2 
  fl 
  

  

  <i 
  <a' 
  o" 
  

  

  | 
  a 
  | 
  

  

  1 
  § 
  § 
  s 
  

  

  5 
  ^ 
  5; 
  § 
  

  

  O 
  

  

  co 
  "S 
  

  

  o 
  

  

  

  

  

  H 
  

  

  which 
  has 
  crystallized 
  between 
  the 
  grains 
  of 
  the 
  rock, 
  may 
  

   have 
  been 
  derived 
  from 
  the 
  lime-bearing 
  feldspars. 
  Having 
  

   no 
  sign 
  of 
  decay 
  nor 
  of 
  distortion, 
  and 
  being 
  moulded 
  against 
  

   or 
  around 
  the 
  quartz 
  and 
  feldspar 
  particles, 
  the 
  hornblende 
  is 
  

  

  