62 



KUIDIIOK NANSKN. 



M.-N. Kl. 



Fig. 3r. Strandllat at Holmen west of Fuglset Fjord. A. Eastern side. B. Western side. 



(Aug. II, 191 1 1. 



mountain slope, and the strandfiat is perhaps still better developed on the 

 opposite side of Sogne Fjord, westwards from Hoiang Fjord. The farms 

 are lying on this plane on both sides of the fjord. 



Illustrations are here given of the ness or rockv point at Ardal, on 

 the west side of the entrance to Fuglset Fjord (Fig. 30), of the point with 

 sharply marked strandfiat at Höhnen, west of Fuglset Fjord (Fig. 31), 

 and of the strandfiat at Akrc (Fig. 32). The height of the level of the 

 strandfiat is at all these places very nearly the same as at Tangen. 



Further west there were similar platforms on each ness and point, 

 and also at some places along the shore between the points, c. g. at Sørcvik. 



At Mafsncs, east of Fike Fjord on the south side of Sogne Fjord, 

 there is a well developed strand flat, forming a sharp incision in the 



' \ 





Fig. 32. Strandllat at Akre. (After photograph. Aug. ii, 191 1 1. 



