﻿r52 
  NEW 
  YORK 
  STATE 
  MUSEUM 
  

  

  Waleott, 
  C. 
  D. 
  

  

  '83. 
  The 
  Utica 
  slate 
  and 
  related 
  formations 
  of 
  the 
  same 
  

   geological 
  horizon. 
  

   Trans. 
  Alb. 
  inst. 
  10 
  : 
  1-38 
  ; 
  pi. 
  1-2. 
  

  

  Waleott, 
  C. 
  D. 
  

  

  '88. 
  Section 
  of 
  lower 
  Siluri?n 
  (Ordovician) 
  and 
  Cambrian 
  

   strata 
  in 
  central 
  New 
  York, 
  as 
  shown 
  by 
  a 
  deep 
  well 
  

   near 
  Utica. 
  (Abstract) 
  

   Proc. 
  Amer. 
  asso. 
  adv. 
  sci. 
  36 
  : 
  211-12. 
  

  

  Waleott, 
  CD. 
  

  

  '90. 
  The 
  value 
  of 
  the 
  term 
  '' 
  Hudson 
  river 
  group 
  " 
  in 
  geo- 
  

   logical 
  nomenclature. 
  

   Bull. 
  G. 
  S. 
  A. 
  1 
  : 
  335-56. 
  

  

  Waleott, 
  CD. 
  

  

  '91. 
  Correlation 
  papers 
  — 
  Cambrian. 
  

   U. 
  S. 
  a. 
  S., 
  bulL 
  81.^ 
  

  

  White, 
  T. 
  G. 
  

  

  '96. 
  The 
  faunas 
  of 
  the 
  upper 
  Ordovician 
  strata 
  at 
  Trenton 
  

   Falls, 
  Oneida 
  co., 
  N. 
  Y. 
  

   Trans. 
  K 
  Y. 
  acad. 
  sci., 
  14 
  : 
  71-96 
  pi. 
  

  

  White, 
  T. 
  G. 
  

  

  '96a. 
  The 
  original 
  Trenton 
  rocks. 
  

   A. 
  J. 
  S. 
  3 
  ; 
  2 
  : 
  430-32. 
  

  

  DESCRIPTION 
  OF 
  PLATES 
  

  

  Fig. 
  1 
  Lyon 
  Falls. 
  The 
  falls 
  at 
  the 
  pulp 
  mill, 
  from 
  which 
  the 
  town 
  

   takes 
  its 
  name. 
  They 
  descend 
  over 
  the 
  gabbro. 
  Locality, 
  

   143A. 
  (See 
  p. 
  r26) 
  

  

  Fig. 
  2 
  Portion 
  of 
  the 
  bed 
  of 
  Dry 
  Sugar 
  creek, 
  near 
  Boonville, 
  show- 
  

   ing 
  the 
  pot-holes 
  in 
  the 
  Black 
  river 
  strata 
  and 
  their 
  enclosed 
  

   boulders. 
  (Locality 
  140A1.) 
  (See 
  p. 
  r28) 
  

  

  Fig. 
  3 
  Swift 
  creek 
  (Robinson 
  glen) 
  section, 
  Chad 
  wick 
  Mills. 
  West 
  

   side 
  of 
  Frankfort 
  Hill. 
  Strata 
  of 
  bed 
  137E2 
  and 
  3 
  rise 
  on 
  

   either 
  side 
  of 
  the 
  creek. 
  

  

  