Xssr wlnda ea»pl«t«ly aoross the Atiftntle Owifta to Europe 

 {24,p,223), wMl© (iust whipped up by wtadstorma on the 

 l&M has been iosown to fall on vessels in mld-Atle ntj.o 



(24,p.243). 



Therefor*;, if iiotieeeble ^iiGOuats of this 

 aust 6r« carried such grer^t distances, uucb larger 

 OBKJunts, ooBtfiiriiug ooerser coast! tu«nts, must b© de- 

 posited over tb© ceerby sbelf , ivooordlagly, th© Selliaig 

 i/irectioas reports fiae «end in Skeidere Dyb, or tJkeidare 

 DJ&p, wbloh h@s been blowei out from &K:@idarlirB8i3dr (18, 

 P.493}. 



(4) -FiaG^io^. Lfeirg© ®ia,©uats of pujaaioe sre delivexw 

 ed to the B©8 by strsems flo?^it^ tkreugh erees of vol- 

 OBuio activity, by gleolwr bursts^ nnd directly by sub- 

 a&riae arupi^ioQs. This occurs ofr otii@r coasts aa well em 

 off the southern and southeast ara, 



-• Acoordias to Vhorodds^n ? 22, pp* 502,505), erui>- 



tions of iiekis (west«*ra edge or £J.^..29S0, on kJtitude 

 64 degrees !:<•) hsv*> produced pumice in nmounts grest 

 enough to be traaspoi ted by ciirrents to the Faoroe Islands. 

 AS previously asentioueci, in 1717 ierge (iusatittes of pumice 

 froa a voloeno in the interior was eerriod to Axer Fjord on 

 the northern coast by the 4f'6icttls8 Hiver ( 22, p. 506 ^« Xa 

 17@3 pusaloe frcot a subisariae eruption off Beykjanes covered 

 the ses for e dist^itoow of 150 to 225 kilometers (2?.,t5.50S). 



