﻿Peiifield 
  and 
  Way^ren 
  — 
  Miner 
  cds 
  from 
  FranMin^ 
  JY. 
  J. 
  353 
  

  

  The 
  name 
  leucophoenicite 
  has 
  reference 
  to 
  the 
  color 
  of 
  the 
  

   mineral, 
  and 
  was 
  derived 
  from 
  XevKoa 
  = 
  pale 
  or 
  light 
  and 
  

   (f)OiiyL^ 
  = 
  purple-red. 
  

  

  There 
  are 
  other 
  minerals 
  from 
  the 
  locality, 
  some 
  of 
  them 
  

   evidently 
  new, 
  which 
  have 
  been 
  partially 
  examined, 
  and 
  it 
  is 
  

   hoped 
  that 
  a 
  full 
  description 
  of 
  them 
  may 
  be 
  given 
  in 
  a 
  future 
  

   article. 
  

  

  In 
  closing 
  we 
  desh-e 
  to 
  express 
  our 
  thanks 
  to 
  those 
  gentle- 
  

   men, 
  named 
  at 
  the 
  beginning 
  of 
  this 
  article, 
  who 
  have 
  gener- 
  

   ously 
  supplied 
  us 
  with 
  material 
  for 
  carrying 
  on 
  this 
  investiga- 
  

   tion, 
  and 
  especially 
  to 
  Mr. 
  W. 
  M. 
  Foote, 
  who 
  spent 
  some 
  

   weeks 
  collecting 
  at 
  the 
  locality 
  in 
  the 
  summer 
  of 
  1898 
  and 
  who 
  

   has 
  called 
  our 
  attention 
  to 
  a 
  number 
  of 
  interesting 
  specimens 
  

   and 
  associations. 
  

  

  Laboratory 
  of 
  Mineralogy 
  and 
  PetrogTapliy, 
  

  

  Sheffield 
  Scientific 
  School 
  of 
  Yale 
  University, 
  September, 
  1899. 
  

  

  