-43- 



As ahoma. on B.A.565 tli« deeps bM hooks fron 

 mat to VBflt are: .^tzwadagruim (stranda Oruad on B.A.29|7)» 

 H&iiAfloa Ojup (H&aefloi Deep on B*a»2977)» Sksits arttnn 

 (aJcagti Gnmcl oa B.A*2977)« 3icag«if jax-dasil^p (SJcagu ?ior^ 

 Poop oa B,^,2977)0 floj&ta Gruim (Strauaiios ?lak on B,A. 

 2977) • J^yjafJaxHAorixi (£yja FjarAsr Pgrb on B.A,2978), 

 Grtasoyiergruan (aria»«y Flak oa B*A,297@)» TJgmeofgram 

 (Ma aoyje Flak ou fi»A.^970)» ^xsrf Jard«r&j4|> (Aacsr 

 FJarder l>yb on B»A,297^}» aiftttugrusn (lielsrekka Flek 

 «i B*A,2978), TliistilfjaTderdj&p (72klstil FJardsr pyb an 

 B.A,2978i, 6 aa Tklstllfjitraar Orujia (KJolson Baiike on 

 B.A,2976}« 



^la» cUMps ar<B fault trou^a, foxxBad^lit lea at 

 as far eaat aa jlyja FJardar Slyb^ fey laovaffieata 8<»i6tina 

 during the I^^Xelstoe^ne epoclk (l?af«277J« Tke deeps 

 east of E^i& FJardair Dyb apparently are related to 

 Iteeent fsultln^; to be deaorlbed later.iSoiaa of tHe wovt- 

 ern deeps laay baire Jswm subjected to glaelal soour in 

 tlielr inner portions as tbeir eorresfKuidlng fjords show 

 evidenoe of slaeiatlon. 



In tbe fjords jbuoIi of ti^e fomer depth has 

 been filled in by sand and silt from tbe large rivers 

 and Btreaas entering at tlieir ^eads (25)« JKnoloaed bastss 

 and tbresbolda, sueJb as occur in tbe Testfirdir bu^ In 

 tbe fjords of tbB east eoast^are ^aotioally laoidn^ 



