PHYSICAL OCEANOGRAPHY OF THE GULF OF MAINE 
973 
A definite indraft into the southern side of the Bay of Fundy along its Nova 
Scotian shore is sufficiently demonstrated. However, this involves only the outer- 
most edge of the Gulf of Maine eddy, the inner part of which continues northward 
across the mouth of the bay, a route followed by some of the bottles. 
Within the Bay of Fundy the water eddies inward along the Nova Scotian side, 
outward along the New Brunswick side and to the southward of Grand Manan 
Island. However, there is some evidence that the latter forms the vortex of a 
second eddy of the opposite sort (clockwise) carrying water inward to the Bay of 
