Lesley.] 



IGG 



[Jan. 15, 



STATIONS, 



+Lake Erie 



Haysville 



Sewicklcy 



Edgewortli 



Leetsdale 



Fair Oaks 



Economy 



Economy Switch 



Baden 



Remington 



Freedom 



Rochester (b) CCCLV 



New Brighton 



Beaver Falls 



Sullivan 



Wallace Run 



Hcmiewood {c) CCCLIX 



Highland 



Summit Cut 



Darlington , 



New Gallilee 



Enon (rO 434 



State Line 472 



Palestine 455 



Leslie'sRun 479 



Now Waterford 503 



Bull Creek 515^ 



Columbia na 555 



Mill Creek 534 



Beaver Creek 487^ 



Green Creek 461 



Gr. Cr. Siding 454 



Middle York 401 



Franklin 506 



149.30 

 1(54.30 

 152.80 

 143.44 

 143.44 

 143.44 

 143.44 

 138.24 

 138.24 

 130.94 

 134.24 

 178.13 

 198 83 

 293.15 

 322.84 

 376.76 

 471.28 

 481.71 

 408.85 

 385.29 

 421.61 



422.46 



Ocean Level. 



722 

 737 

 726 

 716 

 716 

 716 

 716 

 711 

 711 

 704 

 707 

 751 

 772 

 866 

 896 

 950 

 1044 

 1055 

 982 

 958 

 995 



995 



Ocean Level. 



721 

 736 

 725 

 715 

 715 

 715 

 715 

 710 

 710 

 703 

 706 

 750 

 771 

 865 

 895 

 949 

 1043 

 1054 

 981 

 957 

 994 



994 



b Junction with Cleveland and Pittsburgh. 



c New Castle Branch H. R. 



'I Fron^ here on the liKures on page of the Geol. Survey of Ohio, Vol. I, 



1873. Between Columbiana and Franklin is a .station now called Leetonia 

 where the New Lisbon II. U. joins. Neither name nor elevation of this point is 

 given, and therefore no connection can be made with Warren by this line. 



CCCLir. Ohio Eiver Water Levels. 



Elevation of points above tide from report of Col. W. Milnor Roberts to 

 Canal Commissioners, November, 1840. 



Ohio River at Beaver 



New Castle Pool 



Conneaut Lake 



Franklin (a) 



Allegheny River at Pittshurgli (b) 



+Lake Erie 



93 

 222 

 509.50 

 381.50 

 120.50 



Ocean Level. 



666 

 795 

 1082.50 

 954.50 

 693.50 



a This datum is especially valuable in the final determination of the abso- 

 lute level of the Allegheny Valley R. R. sy.stem centering here. But the 



