850 



DR J. H. HARVEY PIRIE ON 



over a considerable part of the snout. For this reason the stratification seen on the 

 vertical cliffs was not seen outcropping here. The extreme end was always hidden by 

 snow-drifts, and partly also by a small terminal moraine. 



The spits which break the regularity of the ice-cliffs here and there do not project 

 any great distance beyond the general line of the cliff. They are narrow and steep, and 

 have always some solid rock showing up at their termination. In some cases this is 

 part of a ridge extending inwards underneath the ice, influencing there the contours of 



