﻿Richardson 
  — 
  Paleozoic 
  Section 
  in 
  Northern 
  Utah. 
  109 
  

  

  From 
  187 
  feet 
  above 
  the 
  base 
  of 
  the 
  Garden 
  City 
  limestone 
  : 
  

   Lingula 
  sp. 
  Asaphoid 
  

  

  From 
  337 
  feet 
  above 
  the 
  base 
  of 
  the 
  Garden 
  City 
  limestone 
  : 
  

   Streptorhynchus 
  minor 
  Asaphus 
  f 
  

  

  Walcott 
  

  

  A 
  new 
  genus 
  of 
  trilobites 
  allied 
  to 
  Bumastus 
  

  

  From 
  375 
  feet 
  above 
  the 
  base 
  of 
  the 
  Garden 
  City 
  limestone 
  : 
  

   Dalmanella 
  sp. 
  Asaphus 
  sp. 
  

  

  Raphistoma 
  sp. 
  Ribeiria 
  sp. 
  

  

  Maclurea 
  subannidata 
  Walcott 
  

  

  From 
  675 
  feet 
  above 
  the 
  base 
  of 
  the 
  Garden 
  City 
  limestone 
  : 
  

   Strophomena 
  fontinalis 
  White 
  Maclurea 
  subannulata 
  Walcott 
  

   Dalmanella 
  pogonipensis 
  Hormotoma 
  sp. 
  

  

  H. 
  and 
  W. 
  Eccyliopterus 
  sp. 
  

  

  Streptorhynchus 
  minor 
  Walcott 
  Asaphus 
  f 
  curiosus 
  Billings 
  

   JEostrophomena 
  n. 
  sp. 
  Asaphus 
  sp. 
  

  

  Raphistoma 
  f 
  near 
  trohiscus 
  Bathyurus 
  sp. 
  

  

  Meek 
  Receptaculites 
  sp. 
  

  

  Raphistoma 
  acuta 
  H. 
  and 
  W. 
  

  

  From 
  the 
  top 
  of 
  the 
  Garden 
  City 
  limestone 
  : 
  

   Dalmanella 
  pogonipensis 
  Hormotoma 
  sp. 
  

  

  H. 
  and 
  W. 
  Echiyioencrinus 
  ? 
  sp. 
  

  

  Strophomena 
  fontinalis 
  White 
  Leperditella 
  sp. 
  

  

  The 
  fauna 
  of 
  the 
  Garden 
  City 
  limestone 
  is 
  represented 
  in 
  

   part 
  by 
  that 
  of 
  certain 
  portions 
  of 
  the 
  Pogonip 
  limestone 
  of 
  

   the 
  Eureka 
  district, 
  Nevada. 
  It 
  is 
  equivalent 
  to 
  the 
  Beekman- 
  

   town 
  fauna 
  of 
  the 
  East. 
  

  

  Swan 
  Peak 
  Quartzite. 
  

  

  The 
  Swan 
  Peak 
  quartzite, 
  named 
  from 
  Swan 
  Peak 
  in 
  the 
  

   Bear 
  River 
  Range, 
  Utah, 
  1-J 
  miles 
  south 
  of 
  the 
  Idaho 
  boundary, 
  

   is 
  a 
  line-textured 
  massive 
  to 
  thin-bedded 
  white 
  to 
  gray 
  quartz- 
  

   ite 
  about 
  500 
  feet 
  thick 
  which 
  lies 
  apparently 
  conformably 
  on 
  

   the 
  Garden 
  City 
  limestone. 
  The 
  following 
  fossils, 
  identified 
  

   by 
  Edwin 
  Kirk, 
  were 
  obtained 
  from 
  this 
  quartzite 
  in 
  the 
  NE^ 
  

   sec. 
  9, 
  T. 
  14 
  N., 
  R. 
  1 
  E., 
  Orthis 
  n. 
  sp. 
  near 
  tricenaria 
  Conrad, 
  

   Eccyliomphalus 
  sp., 
  Endoceras 
  sp. 
  Ampyxl, 
  Symphysurus% 
  

   golfussi 
  Walcott, 
  Bathyurus 
  congeneris 
  Walcott, 
  Leperditia 
  

   sp., 
  Leperditella 
  sp. 
  This 
  fauna, 
  which 
  is 
  related 
  to 
  that 
  occur 
  

   ring 
  in 
  the 
  low 
  T 
  er 
  part 
  of 
  the 
  Simpson 
  formation 
  in 
  Oklahoma, 
  

   is 
  referred 
  tentatively 
  to 
  the 
  Chazy 
  by 
  Ulrich 
  and 
  Kirk. 
  

  

  Fish 
  Haven 
  Dolomite. 
  

  

  In 
  the 
  Bear 
  River 
  Range 
  near 
  the 
  Utah-Idaho 
  boundary 
  the 
  

   Swan 
  Peak 
  quartzite 
  is 
  immediately 
  overlain 
  by 
  the 
  Fish 
  

  

  