«- 81 - 



fiifteec Mlc^s iia wicitii, coiislsting ot sea<?.y nnd f^avftljy 

 fliits, t«sils:e<s tiaeir pi&.©fc, 1M& Is tib,® v'vkmtliea stern Low- 

 ifiaa, jasjatl.oa'ad on pag« 6, Great ©iff ahore bars, becked 

 Isy marshes aad legjoouis, for& tii-a strandlina, Ii©vd.e (12, 

 p.4><B) describes t.ii«»a ©a follows » 



** ...Morer tbeji aOO siiles of tiie south- 



OPS sfaoires or IcelsiKi eojisist ot » great 

 otiBkOT& hhr, TliB Miouiit£.i?iS of the iiin- 

 teriaad fd»Gl3i ths* shorn «& oaiy two 

 poiuta— Ff>rtl«sa<i , south of Ir'iyrdsls- 

 JoJcuIi, aad %hm ¥®stur Eora. Slsewtor® 

 ti].<* f;x'e&t eia'bi«iikfi:ir'int3 of ssnd and aldE- 

 gle enclose wi4s Bi-m&B ox' lagoon, sa««r»h« 

 ianci »m gr«i?el flsita, Jimaeroua rock 

 outcrops ere iaoorj-oysted lu th*^ feiabani!:- 

 ffliaat, fpequ'^-^atly i'ormix-ig uodal poiats 

 tvom vihiGh tka bsaolifes i''«jO«de la swQup- 

 ing ou:rv#» J>ot|i to tfa« «aat aijd west.'" 



FrasB the bfrnk, Breiddels aruna (»•« E,A,565), 

 opposite berufjSrdur, or BrnvM Fjord, soutjuwejit to th« 

 westerja Bide of the sufcmtirii*© valley, Keyais DjSp,or 

 Keyals Uyb, tii® ah®lf n.irrows from ever forty MleB ia 

 vddtfe to le®B tten t®a. It t® iafleated by six large sub- 

 &Bria@ Telleys which, in eeoh, orr*, cause thft lOO-fettiOB 

 depth curve to swini? in helfway or aore aoross the sJialf . 

 jrrom northeast to southw^sst tlies© er© Bwruf jerdBrsll, 

 I/Snsdj&p, Horaaf jsrder Djfip, BreldemerkurdjAp, Slceldarar 

 Djdp, and Heynis Dj&p* 



TiMS« subiactrin^ valleys run up tovn«rd fjords, 

 or toward portions of the co@at where f Joras or ei^cityBUHits 



