116 p. A. ØYEN. - NORWEGIAN GLACIERS. 



may also be seen in the fact that the phase of increase gradu- 

 ally fades away towards the east. 



In the preceding pages, some leading features of the oscil- 

 lation of glaciers in our native country have been sketched. For 

 more detailed information and literary references attention may 

 be called to two reports of the Commission Internationale des 

 Glaciers (Les Variations périodiques des Glaciers. Rapport 1897, 

 pp. 69. 70 and Rapport 1899, pp. 12. 13. — Extrait des Archives 

 des Sciences physiques et naturelles, T. VI, 1898 and T. X, 1900) 

 and more especially to the treatise mentioned at the very begin- 

 ning of this paper. 



The University of Christiania, December, 1900. 



Trykt den 26. april 1901. 



