ALPINE SCULPTURE 267 



trunk formed by the junction of the Eosegg proper with 

 the Tschierva glacier, a short distance below the rocky 

 promontory called Agaliogs. 



This is an extremely slowly moving glacier; the maxi- 

 mum motion hardly amounts to seven inches a day. Cre- 

 vasses prevented us from continuing the line quite across 

 the glacier. 



