- 62 - 



The d4M»p8 W9TB probe ttly cut by subserial 



•rosion when %h& akBlt was 0(^pletely exposed at the 



end of the Plioo«jci6« As far as %h& author is aware, 



faulting J&as pliiyed no part la tlieir fonaatlon. SQm» 



deeponijag may JtiaT^ T&^ma acoompIlAhed by glecJbeX oxea- 



fbtion durizig the Pleistooane epoeiif however* 



^klctt Fl&l Byb end YoBa« Fiord. Bsthyagtry and 

 Bottom aedliasnta 



Bfijcke FI<lii Jli^b extends aortheestwsrd tTom. 

 the bay, Bek^ 71&i. Its ^p!>efitest ^aeasured dc^pth, 20B 

 fethos&a, fells outside B«A.297Si on which chert most 

 of the bottom lies betvieeii 110 &m 150 fathoms* At 

 its shoreward end the deup turns southward toward Vopne 

 fjord, tvhile a aoaller br^iieh shown by th@ soui^diags 

 ooQtlimes eouthwestwerd eat runs up into Bekice FlM. 



Much of BBKk& FlSi I^b is floored with Biud, 

 particularly the deeper central portions. It i» not cer- 

 tain if this aud forms a continuous belt, as shown on 

 the ch^rt, since sediiaent notations are widely seper&ted* 

 ^nd oorers the slopes on the northwestern side of the 

 deep, and the slopes and part of the bottom on the south- 

 ee stern side. 



The shorewerd end of Bakkn Flhl I3yb is, to a 

 greet extent, surrounded by grevel* fhe boundary between 

 grevel end maA on the ee stern side of the southward ex- 

 tension of the aeep, at about lifititude 66 dej^rees 7 oiflK 



