﻿W. 
  J. 
  Miller, 
  photo 
  

  

  View 
  across 
  the 
  Hudson 
  river 
  from 
  a 
  point 
  just 
  south 
  of 
  the 
  railroad 
  

   station 
  at 
  Riverside, 
  and 
  typical 
  of 
  the 
  region 
  through 
  which 
  the 
  river 
  

   flows. 
  The 
  mountain 
  consists 
  of 
  quartz-syenite. 
  The 
  Glen-Riparius 
  fault, 
  

   which 
  the 
  river 
  follows 
  for 
  some 
  miles, 
  lies 
  along 
  the 
  base 
  of 
  this 
  mountain. 
  

  

  