94 



I KID I I OF NANSKN. 



M.-X. Kl. 



Fig. 78. Panoramic view of Karmoi and the mainland, taken from a hill north of the bay at Angval; 



of the u 



aBÊÊÊÊÊl 



Fig. 79. Karmoi south of Hoge Varde lighthouse, with hills rising above the plane of the standfla 



(Aug. 31, 191 1 1 



On the islands south of Renncsoi (Ulfstcin Island and Fjolloi), there 

 is a well-developed strandfiat. The sketch Fig. 84 demonstrates how the 

 almost horizontal plane of the strandfiat extends to the foot of the moun- 

 tains Byrefjell and Kneberg-, which rise abruptly above this plane. The 

 rock is granite on both islands. 



The strandfiat has a wide extent over most islands in this region 

 north of Stavanger and out in the sea to the west where all islands are 

 low and very flat. 



Kz'itiii[^soi with its hundreds of surrounding islets and skerries has 

 a very conspicuous low flat level cut in chlorite schists (Fig. 85). In the 

 eastern part of these islands where the view Fig. 86 was taken, the average 

 height of the plane was measured by levelling to be about 9.5 metres above 

 the sea. But the level at which the farms are lying farther westwards (see 



