• « • 



■ow «xt«ad mitwttrd froa tJH» Bftia b&y and fjords (««• in- 

 4«x eiiavt B*A,56$tw9r« out «t %ixat tlm«»wliea tlie sliAlf 

 wai0 ezpo«e<l to Stt1»««rlal «r9aioii* 



aid«ct Bgaia uaiil tlu» streak liaa lay et cteut %h9 «hm 

 Ittiral «^a it aid INfoz-e; i«a« 100 «M»t«re or £Sor« slxyve th« 

 £^ar«0«at streM line. Agsia, 6a before, sluill beds tvora 

 dap9ait«A at tlia higHast Xtv«l« Tiiaa® data tke tis&B of 

 sazliittBi r«-6ate«rg«ii«e as aid-^lelstoe^zi^, aiaa® tt»t 

 tlma tlM XaM m» hm^&. aautrsiii^f «itii ii^Xta Xo^ ^"t'ntfh 

 to pazmit %h9 tenrntion of aavsral m^^rlne terreoaa* 



la tii« Fl«i$toe<»a& apoeft at laast twise «Imi 

 antlra isXaeo. was ■-r-.V'-.rM.-;i .^,7 ».» ia»; »h**>fjc t-firo^,.-; ^'fSiiob 

 a few paaJca proJact«>S» >^it ^x* areealead to4&y, •r.^i-s lo« 

 ootrared tiie eo&atsil Xowlaada aad api>a7®Btlf 9-s:%i-:u4,*&d 

 past tJia p7e8axi-& atr^M Una, aa Xarga - asbounti^ of ^:;o?«fd.ii« 

 have Immi found at varloaa pii^on^ oa tito aoabotto^'. c^ff 

 %h» notttlia of tHa f jorda* 



TuXaeniaai, wnlafe waa aatiirft duriai; tb» aarljr 

 and middle part of %&® 'lartierr? apparvRtXy ooaoad dtirissif! 

 t^a PXiooeaa epoab uatiX tlktt period of aaarfeiia«) at the 

 OAd. It tliae. iBjrolca fortl&, •nA doriae tba flaistooaisc^ 

 a amlMHr of Xare« fotoaooaa wer$ «otiTa« THis aetivity 



