Ordoi'icisk tiler Vmur- 

 SiMir(HeJcl<i-huk Formasjon) 



^T-A Granlit og Gntis-grcinlttj 

 y+^ sansifnliß Fra. SiLvr(eJïir/^ocl) 



so 

 ' ' I ' ' "^ 



100 km. 



56 O 



Sifclkjxpp 



Fig. 135. Geological Map of Spitsbergen, chiefly after A. G. Nathorst, based on the Swedish, Rus- 

 sian, Scottish, and Norwegian researches before 1910. The broken and the dotted lines indicate 

 the course of the "Veslemoy" in 1912, with the océanographie stations. [From Nansen 1920]. 

 Translation of the explanation in the lower left corner, i Tertiary. 2 Diabase. 3 Jurassic und 

 Cretaceous (Neocomianl. 4 Trias. 5 Carboniferous and Permian. 6 Devonian. 7 Ordovician 

 or Under-Silurian (Hecla-Hook Formationl. 8 Granite and gneiss-granite, probably Post-Tertiary 



(according to Hoel). 



