164 FRIDTJOF NANSEN. M.-X. Kl. 



to l)c an cnicrj^cd strand flal . I'ut on tlie wliolc there are very few such 

 formations alone; the coasts 01" !• ininarken, whicli as a rule is extremely 

 steep on the outer, seaward side. It is, however, possible that the low 

 land extending along the coast t'roni \ ardo to \'adsø and along the north 

 side of Varanger l-'jord may be considered as a strandflat, as Reusch has 

 indicated on his map [1894]. As I have pointed out [1904, p. 119] it is 

 also possible that there are indications of an emergerl stranrlflat in the 

 inner parts of the I'inmark h'jorils, e. [^. in the inner end (jf Porsanger 

 h'jord. 



