Feb., 1914.] 
Flood Erosion Along Paint Creek. 
253 
At the extreme southern end it terminates by narrowing into a 
small, shallow gulley, a foot wide. The sides are perpendicular 
and appear as if trimmed by hand as is shown in the photograph. 
Fig. 2. Exposure of the cut wall and the dolomite. 
The walls show characteristic glacial drift overlain by a thin, black 
soil. Beginning at the northern end for nearly half the length of 
the cut all the material has been removed down to the Greenfield 
dolomite. 
Fig. 3. Re-deposited drift in the pasture. 
