A FIVE-YEAR FARM MANAGEMENT SURVEY IN OHIO. 7 



easily, and for this reason much damage has been done by washing. 

 On the whole, the type is a rather strong soil, and were it not for the 

 steepness of the slopes and the difficulty of cultivation it would be 

 prized much more highly than it is. 



Under the residual shale and sandstone soils another series of soils, 

 designated the Meigs series, has been established. It represents a 



Fig. 3. — Scenes representative of the, topography of Palmer Township. In the upper 

 picture the surface features grade from rolling to hilly, with steep slopes occurring 

 here and there. In the lower picture the greater part of the surface grades from 

 hilly to steep, with occasional small areas of rolling or plateau-like land near the 

 crests of the slopes. Approximately one-half of the entire surface of these farms 

 grades from rolling to hilly, and one-third from hilly to steep. 



gradation between Dekalb silt loam and the Upshur clay, or a mix- 

 ture of the materials constituting them. 



The farmers' estimates of the proportion of their farms repre- 

 sented by each of these soil types were as follows : 



