- 44 - 



in the f jorda of Xh& north eoast* 



tjtrfcinda urund. ifetlivx'iQtry and BottoaB aggjiaents 



The eesternmost of the hanics, ^stranda Gruad, 

 extends slightly over fifty Mies north«a«tw&rd from 

 Morth C«p«, AXoa^;, its nortiii»rn ©dgs it is oov®r«^ with 

 mixtures of laud, si^na, una gravel, Between this outer 

 zone and Biorth Ciap@ the ohidf sMiji^nt is aand, contin- 

 uous with thtt s^nd ooTering the shelf off the western 

 ooast of Iceland, 



Th6 entire aoutheast^xn half of strand a 

 arunci, from the coast out to th@ northwestern end of 

 the hanic, ia covered with gruvel, forming a gr©®t 



irr Similar- shaped belt papelleliag Hiinafldi D©«p, A 

 10 to 15-iail© udde aone of rocJ^ r0®fs and shoals, eellefl 

 ^trcndahrekar, extends alcaost completely across this 

 grevel belt at its ahoroimrd end* 



Thp®e shoal patches in th© vicinity of 

 Xetitude 66 d8gr<@es 21 minutes IU» I.oneitnde 21 dogr««s 

 50 minutes *Am be«r mud notations, fh.^^- author believes 

 these may b« of glaoial origin* The sinuous, esker-like 

 ridge 8t iifititude 66 degrees 23 minutes I^t• ,Lon«i!;itude 



22 degrees 2 minutes w, and the enclosed basin of Dran^p 

 All at ^^titude 66 degrees 2? minutes N., longitude 

 21 degrees 50 minutes u, liicewise are features probably 

 produced by g3.tiCi£tioa, 



