58 



KKID'IJOF NANSEN. 



M.-N. Kl. 



Sita/ietfUU at Mflmam- 

 veti , LeikariffeA, 



Fig. 22. Sogntlal Fjord and Noruin Fjord, in the inner part of Sogne Fjord. 



At Kjørncs, the flat, rocky point (crystalline scliist) between Sogndal 

 Fjord and Eids Fjord, there is a \ery level plane cut in solid rock, and 

 forming a distinctly marked incision in the mountain slope (see Fig. 23). 

 The level of its flat surface is 9.84 metres above the sea. 



At Pallenes, in Norum Fjord (Fig. 24), a distinct horizontal ledge 

 lies at about 10 metres above sea-level, anrl is the same formation as the 

 l)lane ol>served at Kjørnes. The rock is here gabbro. 



At Vines (gabbro), farther out in Norum Fjord, a distinct plane is 

 cut in s(jlid rock forming an incision in the luountain slope at about tlie 

 same level as at Pallenes anrl at Kjornes. The small islets, the \'ines 

 Holms, outside the shore, form a continuation of this plane (see Fig. 25). 



The small peninsula, on the other side of the fjord, just opposite the 

 Vines Holms, forms a vcrv distinct strandfiat at an average level of some- 



Fig. 23. Kjørnes Point, between Sogndal Fjord and F.ids Fjord. Strandtlat 9.8 metres above 



sea-level. 'July 29, 1911). 



