- 63 - 



utes K,, jjongltude 14 degrees 23 miautos w,, hes beea 

 placed along tlia bottom of a pronouiiosd break la slone, 

 wii>!>re . viie ooi^toia falls off vo wie west ovex >u raiiiicsas 

 in 1 mile. 



This gravel ia probably ooatinuous with the 

 grevel surrounding Leziganes /lak. It also extends to tile 

 soutli sad east, covering most of the bsak cr-llsd Vopaft- 

 f jsrdergruim on B.A,565. 



The large axet»s of saM in Baicfca Floi aad Itt 

 Vopaa Fjord, 20 miles to the south- southeast, have very 

 likely been deposittid froa th© streasis ©ntsriag at their 

 heeds. 



The bottoia for 2 miles to seaward from the 



peainsula southeast of Bslcka Fl&i is rocJcy. IJ,k9wis«, 



rooii bottom extends aor© thea five iiiil©s outw&rd from 



the peninsula betweejh /opaa jjord end Hjireds Jl&i. 



Hjirada Jl&i aiid Hjirreds Flhi Dyb. Bsthyaetry and 

 BottOB Sedlmeais 



Hjirsds Fl&i, southeast of Vopaa Fjord, and 



jij^rade flo4 Dyb bt^ aeeward extenaioas of two long, 



nerrow valleys which ooBaaeaee la the interior &nd merge 



into one lowland just before resohing the sep. The jS- 



Jculsa aad the Lager fljot idvers, which flow through 



the vslleys, both head in Vetna Jckkiai. Both velleys 



