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u0f f shore • jk;xfiiapl@8 ot t'ae»9 are: Diana Bodi (latitude 

 65 diigroos 3*5 minutes N., Longitude 13 degreita 12.5 

 ainutes ll.), Nyibodi (latitude 64 degrees 50*23 min- 

 utes N., Lonsitude 13 de^@«>s 26 miautes W. ), ^nggar 

 (Ltdti^ude 64 d«gro«8 42.23 aiiaut^s H. , longitude 13 

 degrees 25,5 adnutea «/•), Hvslsbelcur (Latitude 64 

 degrees 36*25 miiautes N«»Loiigitude 13 d€«ree» 17 lala* 

 utes W.), Istlbodl (Latitude 64 degrees 35 minutes H*. 

 Longitude 14 degrees 3 liiiiiutes ii,), and others. 



th» eolAOideao© of most of these rooks with 

 the belts of gravel previously d&sorlbed lends weight 

 to the hjrpothesis that th@ grevel was obtained bjr weve 

 erosion on rocicy terrain when th« seslevel wes lowered. 

 The rooks would therefore represent unreduood stecks 

 and ledges. 



The abnorx.i&l loagnetio variation noted et 

 Diens Bodi end other pleoes along the eoi^st attests to 

 the ferrous ns^ture of the basic rooks underlying? the shelf. 

 The CoeatliJUKfe between Heaers yjord and Yestrahorn 



In Hemars Fjord and Alfta Fjord, southwsst of 

 Beru irjord, no Infori^ition is evaileble as to the nature 

 of the bottom sediments. A send ber 6 siiles long hes been 

 built ooaapletely across th® mouth of Alfte Fjord end pert- 

 wey eeross the loouth of UasAsrs Fjord. This is the first 

 of a series of great offshore b&ra and storm beeches 

 fringing the southeastern, southern, and southwestern 



