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DEPARTMENT OF THE NAYAL SERVICE 



In a similar manner, we should be able, from the movement of the water, to 

 ascertain the stability of the same. If the water flows parallel with the coast, it is 

 stable; whereas water setting in towards the shore will be homogeneoiis. On the 

 eastern side of Newfoundland, for instance, the water flows np into the bays (vide 



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 03 



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fig. 28). From this we may conclude that the water here is of but slight stability. 

 On the southeast coast of Newfoundland, on the other hand, the water sets outwarda 

 from the shore, even occasioning a reverse current in towards land. Here, therefore,, 

 the water is in stable layer formation. 



