AUBURN. G 5 . 155 



opened in the lower members of the CatsJcill sandstone se- 

 ries principally in the New Milford Lower 8.8. ; one of these 

 near Lacey ville has an elevation of 200' above R. R. there or 

 (658'+200)=858' A. T. 



Jnst below Lacey ville on the east bank of the Susquehanna 

 may be seen a vertical cliff of Catskill rocks 200' in height, 

 and the New Milford Lower S. S. occurs near the top. 



Fossil plants. — At the flag quarries we often see many 

 fragments of vegetable remains broken and macerated be- 

 yond identification. 



Along the stream which enters the Susquehanna at Lacey- 

 ville we see many fossil shells of Chemung type coming in 

 about 150' below the New Milford Lower S. S. 



Barometric elevations in Auburn. 



A. T. 



Forks near J. M. France's, 1470' 



" Benjamin Canlield's, 1465' 



" J. E. Hibbard's, 1430' 



Level of Riley creek near Harris's mill, 1125" 



Forks west of J. Murtaugh's, 1330' 



Forks near Mrs. R. Black's, 1260 



" Bennett's hotel, 1360' 



Cross roads in Auburn Center, 1390' 



Forks near I. Scott's, 1440' 



%t John Carlin's, 1050 



Level of Little Meshoppen near by, 1000' 



Forks near Caldwell McMicker's, 1300' 



Cross roads in South Auburn P. O., 1200' 



" near D. Dornblauser's, 1140' 



Forks near N. Baldwin's, . 1125' 



28. Scott, in Wayne county. 



This township occupies the extreme northern portion of 

 Wayne, being bounded on the west by Susquehanna county, 

 north by Sullivan county, New York, east by the Delaware 

 river, thus extending entirely across the north line of the 

 county. 



Trending north and south through this area, in a very 

 irregular line, is a high divide ranging from 1800' to 1900' A. 

 T. The K Y., L. E. & W. R;R. (Erie) crosses this same 



