360 CHARLES: S. PROSSER 
It will be noticed that the cliffs increase in height as followed 
eastward from the Lake Breeze House to Eagle Cliff. The cliff 
at the Goetz house, one mile northwest of Eagle Cliff, is nearly 
38 ft. high and the one just west of Eagle Cliff 473. These higher 
cliffs also show a greater thickness of the Cleveland shale, as, for 
example, 34 ft. in the Hinz Cliff, 193 in the Goetz, and in the low 
cliffs near Lake Breeze only a few feet at most. 
Fic. 7.—Cliff at eastern end of Eagle Cliff Park on shore of Lake Erie. Upper 
part of cliff Cleveland shale; lower part Chagrin=Huron. 
A view of the shore of Lake Erie at the eastern end of Eagle 
Cliff is shown in Fig. 7, where the upper part of the cliff is composed 
of Cleveland shale and the lower part of Chagrin= Huron shale. 
The cliffs along the lake shore from Eagle Cliff eastward to 
Rocky River, the banks of this river, the lake shore cliffs in the 
western part of Cleveland, and many sections on the streams east 
of Cleveland have recently been described in Bulletin 15, 4th series 
of the Geological Survey of Olio, to which the reader is referred for 
a detailed description of these formations in that part of the state. 
