1 92 1. No. 1 1. 



THE STRANDFLAT AND ISOSTASY. 



167 



Xo^^l^a^pf; 



fCaafi 



Kf/eintiu. 



Xopsfci hÆ-onJitr- 



y no uin'tc Kail -Cid 



Pld'tC ,(HMc/CuU-tui 

 ]TuiicU.yuc kcUk&Uyi.) 



qui Aam^t£7t mtxiko-nûlo- 

 'm eA-aU-fi^, ^Q/ri^nl -nUl/ie. /Cull. 



[Miltc 



chue cUZ, mtôl kcUkått-n 



\KuU-t. i^ai-^ic ciU -KLeit tod baniteii 



\ {zia^iit. iikkc. Scon-iten cfk ifkfälc ndr 

 j ) med kuU-lo^ tn-evL ^ki/b i "^ 



Lofi^tie. Ouùn^<cjKc I ncKLu -Ituk. 



Hg. 125. Geological map of Bear Island by O. Holtedahl, based on his investigations in 



1918, and those of J. G. Andersson in 1898. [Holtedahl 1919]. 

 Translation of explanation, to the left : i Trias. 2 Younger Upper Carboniferous (Spirifer- 

 Cora-coral limestone). 3 Older Upper Carboniferous (Fusulina limestone, &c.). 4 Yellowish 

 sandstone with conglomerates, probably Middle Carboniferous. 5 & 6 Middle Carboniferous. 

 5 Upper part chiefly limestones with limestone conglomerate at the top. 6 Lower part 

 chiefly red sandstone and conglomerate. 7 & 8 Lower Carboniferous and Upper Devonian 

 sandstone series with coal seams. 7 Chiefly sandstone. 8 Sandstone often interbedded with 

 shale. 9 Tetradium limestone. Middle Ordovician. 10 Younger dolomite series, Lower Ordo- 

 vician. 11 Slate-quartzite series. 12 Older dolomite series, presumably Ozarkian. 



9 — 12 Heclahook System. 



Explanation to the right : i Faults, probably older than the Spirifer limestone. 2 Probable 



faults of the same age. 3 Faults younger than the Spirifer limestone. 



