42 
Frank Carney 
That the intervals of these benches are connected genetically with 
the more continuous shoulder and terrace to the north is not estab- 
lished. Furthermore, the discontinuity southward of the better 
developed cliff is possibly due to the vigorous ice-erosion that 
altered the lower horizons of the walls of the longitudinal valleys. 
No. 2. This bench and terrace first shows about two and one- 
half miles north of Dunning’s Landing. It is remarkably con- 
tinuous (figs. I, 2 ), and generally sharp in development. At one 
Fig 3. Shows a lateral moraine which crosses the middle and highest terraces, 
and descends to lake level south of Ogoyago. 
locality towards the north, where the eastern slope of Bluff Point 
blends into the northern slope, the twelve foot horizon of shale, 
mentioned in preceding section, was noted; here the shale is nearer 
the top of the bench; not much importance, however, is attached 
to this vertical position, further than to note that it could have no 
genetic association with the bench. The original relationship of 
terrace and cliff, so far as analysis of a particular cross-section is 
concerned, has been given much indefiniteness by the agents of 
degradation; whereas this relationship is still conspicuous when 
viewed from a distance. 
