. 7 • 



«»t»r» elttvatlem ebove tho sm®. Its oois^tXlaA |« 



t>h<» oliffsd plat«ttu e^l^tt. For oociv«ni«>ao« this p«aia8ula 



is <iall«d In this r«port tiie Northwestern B»£LlaeuIii« 



Xodlaaa is « r«isaasit ojT a voleanio plate^ta 

 wladoli, durlM ^c^rly Tertiury tlmos prol»abIy speuiied 

 t>b« •tttiro North At.la3tla« This platoiu lit la«li«!V<i4 

 to li«vo 1»o«a brokexi a|i by bl<3ok fa\U.tlJig aM vttbsid* 

 oaoe in %h9 Mloeeae speoii wliio^ l&t% loelaM sa isXaod 

 witJa its «o«sts 39 to 50 miloe fttrtker out on ^li si<i«s 

 t&on aow* Other r«Hm«ata of tlii» plateau srs the 

 ifsoros Xslsads, the isXsMs of {lull aaa SHqto off tho 

 •y9St«ra ooaet of SootlaM, AatriiB in laorthomstera Xrol@M» 

 CAd ths besait 7»gioa of oiestoru Qrm&aliiixd, 



^bsid«ao« ooatinu^d tnrou$M th@ PXioeone 

 ujatiX tho strsad Xin® -sms o'v^r 100 a^t^r^ a\!»ovt th« 

 proaoat strahd Xiii«, ShtXX-bo/srin^ bsds of a^adstoas, 

 whioh oorrsXsto tej3t«tlv«Xy with the 3XiOtt«a« Bod Crag 

 formatioa of EngX^nd, W9r# d«posit®d at this hifii Xov«ti« 

 ApparontXy the isXead 8h«Xf was pXaaed by wave aetioa 

 during ^J^A poriod of subsidano^* 



At tho aad of th« FXiooaaa apooh tk» laXend 

 was 7«*«l«<fated untiX tha »»& had retraatad ba/oad 



