thi& &vtTf» »M th« sko7« hM9 1t«<»n ^fiplotoA fta sandy «m 

 th« basis of tbt iSfiSid-bott^ft symbols ui«#d on t&le! sbmrt 

 end Qfi B, A* 3201. 



Si|at of .Lon^ltua© ^ a@^rr«SS 21 rfllautes W, 

 th» iMittsra of aedtesnt y.oat?« Is ®x««?'«iair»rT^r 5ore^l.*ix, 

 r^fiteOtlBf. tine iir«at«r <S»t«ll portr«yed oa in^ .. --f' 

 «c«il« ofaerts B,A»5201 isnd B,A,2729. If the port! 



?iaX6?fll»l west of thet acridi?,n w@p« Phown oq ohr: -. _ 



volved 1^3 it In ©est of it, 



/.a irrtf-rjlf r belt af ^avel 2- Mtf^s wia« 

 fci Its widest \.t&iiaii ^Ixifiivul^ m^Bt of mQTX.U toi IX 

 .viil®» fro» XiStltude 6U a®gr®»® 3«5 ali|»it®» K^.f/jm-i^vi^s 



22 dtffr««s 6 ffiJ.rmt«9 W. past the laou.tSis? of !fef.n*ff f»?^i» 



Loa(<!,itud# 22 detgr^es 4 mia^atss W, H#r* It jaiae ot 

 sd-.-^olnt » belt of ^sv«X of siiailaT' ti-f^th ruaalajt? 

 «ia3-&-we8ii ena i/iag partwajr fitsroiss t&<& aout.ii of iS'^sl- 

 f^Sx-ds. A sisillsr feslt of gravel lids di:r»etlj ^tliiwsrt 

 tiie laotttlk of tor^arf j5rdr. ^li«aa th-"f->-s. .tsv«1 b^lts asy 

 Tttpresoat aorui^sl suitsriel 4«i|^sitdd iijr (|Xa6i«rs Tot^ 

 iik^Tly ocQupyiiiK the. .fjords, possibly prior to submergence 

 of the region. The areas covered by them are not notice- 



