- 46 - 



Mixed saad and oud occur tiarougtujut. its Xen^tit, Vh9 



wtd l8 Bo9ggiId*s €^ayt deep-aea eley (9t^^3^t 3,Plete I) • 



Hunafl&i Qm&j? rims southward up into Slcai^* 

 strand Bay, lH»twt«A tli« Hortitwastara Peninsula ana th« 

 peninsulit ol akagen. This, In turn, bifure^itf^s into Hrute 

 irjoj»iur on tb» west encl Huns Fjord on the e&»t« 



A i^rrow iatJbfflStta, iwssuriaf" 4 aiiles iji wi<lth 

 sad 228 fflsters in oaxiisum height above set^Xe-veX, oepeT&tem 

 Bitru Fjord, west of th« siouth or Hruta Sjordur, end Oils 

 fjord, at the h«®d of Br®idi f|ord. If this isthmus w®r« 

 not present thd l^iorthiisfltorn Poninsulis ¥<rouXd h® «n if^land, 

 The orients tion of Bitru fjord and Kollm Fjord suggests 

 that the inferred northe«st-tr®ading fault syst<»ra of 

 &reidi J«'jord {»»& p£ig« 2@) may out across the iathsaia 

 £tnd intersect or mergo with th® system outlining', Eruta 

 fjordur and HunaZlk&i DcMip. 



Thd 2suid in Htthsfl&i Deep is ahflwa as extending 

 southward to the mouth of Hrut® Fjordur, Thiu is consid- 

 ered to he a continuoua bait following the chennel that 

 TxuiB into iiruts ijordur* 



A aaaond, narrower heX'» of mud lies slon^ ttit 

 axis of the Inner half of Hruta JTjordur. The sandy araa 

 on either aide of this belt, and possibly the bait itaai f , 

 conttiino sholls, in contrast to th«i Vestfirdir (sae pat* 

 3S)« One possible explanation for this may be that tha 



