GlettiAijeneagrbum (se« xi.A.:>&5)* @s outlined li|c the 100» 

 fstihoa depth curve, reaohes over forty lailas eaatwsrd 

 tnm the oofij^t* narrowlag froa 20 miles in width et the 

 shorem&Td bqA to e poiat at th@ outer @ad. South of it 

 the doep, Soyiisf jardardjAp, with th® floor lying, for 

 the most part, betw®oa 110 and ILO fathoms, extends eest* 

 werd ttou i»«ydisfjSraur, or 3eydis fj©rd» A loiijs, a»:jrsow, 

 unnemod benk extending eastward from the vicinity of 

 Hj&fi :Fjord bounds Seydisf jerdardj^p oa the south. 



iTo&k Hjerads Fl&i to seMvik Ci.8titud® 65 

 degrees 5*5 i^iiut^s H,,I.oh<gitude 13 degrees 32 oinuteslf.) 

 eaiid is the predomiii'Bht sediment, ooferiJ^^^ deeps aM 

 banka alike. However, areas of gmv&l ooeur ioceliy on 

 the beaks. One erea, measuring 16 milee east-west }aiy 10 

 ffiiles XLorth-south, occupied the west central portion of 

 Glettiageaeegrunn. Another eree, measuring 9 milee essV 

 west by 4 isiles north-eouth, lies on the banlc eouth of 

 ^eydisf jerdsrdjdp. One «Bell ares of mud of unknown size 

 lies in Seydisf Jardwrdjiip. 



The coast, both in the fjords end on the 

 intervening: peninsulas, is fringed by reefaa, whila lao 

 leted rocks and patches of rock bott^om occur at various 

 distencee offshore .Grevel eovers thf» bottom for 6 miles 

 out fr<»a the peaineule between Seydls yjord sad Mj&fi 



Fjord. 



