- 57 - 



the heed of Sic J&lf audi, b«ad® at the aorthweat«2>n &d&» 

 of th« io€t Ali««!t ?@tna J&fcull, 100 Mies to tHe south. 

 Aoeordiocly, ita weters dollTer gr«^t itmoimts of glacial 

 Hilt to the S4>6, as well as sand ^ad imaioe derived 

 from the voleanio ragloa through ^e^oh it flows* 



MaaeyJar Jlaic. Bathyaetrv end 3k>ttoia ;iediM^atB 



This bank <@3c:teMs 23 milaa northward from 

 tho peaiasola of Tj^ties* 



It hoars two rooiqr ahoal p^^tohea! Maa&reyjar 



{Letitude 66 degrees 17.5 Minutes H. .Longitude 17 



degrees 7 minutes w. ) and J^JarhralckB (Latituda 66 



degratsa 19*5 Hiiiiutas M. fLo^i^itude 17 dagraas B BtiuutasW.}. 



Oraral eurrounda these shoals ao^ axtaMs along tha 



bfiokbona of Maoayja Flak in disoontinuoua halts sad 



patches to v^ithin 10 miles of the northern and of the 



h&ak* Th« gr^Tal surrounding Manl^rayjar, and perhaps thc» 



sraval furthar north also, is hallavad to have resulted 



from sulamarina Tulesnlaau Caravel skirts the northern 



coast of the TjBrnes peninsula, forming a Ig-oile wide 



hand. This can prohehly he attributed to wave erosion on 



the rociqr coast. 



Axay gjardar JPyh end Axsr fjord. Bathjraetry and 

 Bottoa Sediaeats 



I^y^in^j: between ^aneyja TX&k and Malralcka Flak, 



this deep treads north-northivesttrord froa .^«r yjord. 



It apparently coalesces with ^jllfaadi Sgrb about 



