FRIDTJOF NANSEN. M.-N. Kl. 



Acor'IiiiL;' \'> wlial lias hccii sai<l al)(»\c, llic low lc\cl rc^\(i]] al the 

 iiiiKT cml of ( liristiaiiia l-jonl, may he considcrcfl to be a rej,^ular slranrl- 

 flat formed in a manner similar lo llial of the west coast. 



W'liellier there are two différent le\'els, or even more, in this rej.^ion, 

 is ili ff icult to decifle, l)ecause the (jrig^inal plane or planes have been mfjre 

 disturbed bv the late j.^lacial erosion than those of the strandfiat of the 

 Norwej^-ian west coast. Another flifficulty hampcrinj:^ the investigations 

 is also that the strandfiat in the Christiania reg-ion is almost everywhere 

 wooded. 



Although it mav look as if there are indications of at least two levels 

 in several places, \ dare not express a definite opinion without having 

 made more careful imestigations. 



