- 49 - 



M^^ aay 1M» residual from a former %iBM of lowered soa- 

 level* 



Irrogalar- shaped t>«lts of send lie on either 

 side of the north- treatiiag oentral grarel bolt, covsrior 

 th@ reaalMer or th« baiik exempt fo^ the outer end wlitM 

 itt&d is t^«L prodcoaiaaht s@diM®iit» Tho sand belts* la tum» 

 :;«re flanked % the sm& of Emi3$)fl&i:Deep and Skega Fjord 

 jpeep* Two l80lati»d, liaear^ahep@d aroes of send extend 

 north-northe&stward along th© e@ stern and imstera sides 

 of the heak at its outer end, 



^kae» fiord Deep. mtt^m&Xry end Bttttca Sodiaieaf 



This deep is well-defined out to ebout Letitttdo 

 66 degreos 2? sinutes X.* re^ehlng l^d tB%h<xsm there, fjto 

 isoleted sttbmerina ridge» lie ia the vicinity of T^titiiae 

 66 decrees 20 adautes U, the Ofisternssost of these rises 

 4S> fcithoias above the eh&nn@l east of it* n^iile the wesV 

 ernmost rises from 10 to 30 fathoa&s sbove the sui>roandimi^ 

 bottoa. They ixmy be due to faulting* espeoially the vw8t'-> 

 emiaost, whioh ia limear-ahaptid, or they toBy possibly 1» 

 due to glfioial depoaition, 



&kegfi Fjord ^eep 1st floored with mud southWBSrd 

 to I'StAtude 66 degrees 5 Binutes H. Flanking it on the 

 •est* along; the edge of i;»tra«raR«s Fink, is e belt of 

 send from ih to 6 olles v^lae. <Btrau»&e8 .rlak itaelf is 

 covered* for the ttost p&rt* with grevel* thus eontinuii^ 



