- 27 - 



Investigation follows: 



(a) All of the drift bottles indicated w tendency of the waters 

 to circul-ate the island of Gr^nd Mnnon in « clockv/ise direction o 

 The complete circuit of Gmnd Mnn«n is not suggested by the results 

 from «ny one bottle „ The physical n«ture of the bottom to the south- 

 west of Grqnd MTinn is orobnbly responsible, "s it hos been previously 

 shown thot the surf nee wnters to the southwest of Gr<and Monnn cir- 

 culate in an '^ntl-clockwise direction. 



(b) The movements of the bottles suggest 9 cyclonic circul«ition 

 about the b^sin determined by the 50 f-^thoms (91 m.) contour in the 

 Bay of Fundy, 



(c) An Intense movement towards the mouth of Prtsspimaquoddy Bc,y 

 is definitely illustrated, while it v/ill be noted th-'t the v/nter 

 movement along the co^st of Cqmpobello Island is outwnrd. 



(d) An inward movement in the m?? in wnters between Grand M^n^^n 

 nnd the ras^inlgnd is noted in keeping with the clockwise circulation 

 about Gr^nd Mnnnn, Hov/ever, the wnters in contact with the const 

 of Mnine hnve nn outward movement. 



Annual Varintiong in Temperature and Salinity 



Vftrintlons in temperature ^nd salinity thn t occurred in the Be^y 

 of Fundy between the years 1924 nnd 1930 inclusive, sre illustrated 

 by reference to data obtained monthly from Station 5. The vari- 

 ations in the conditions of the more stratified and deeper waters 

 toward the mouth of the Bay nre illustrated by observations made at 

 Station 3 (M'^vor 1923) between the years 1916 ^nd 1918 inclusive. 

 The locations of these st-^tions are shown in figure 15, 



