96 ARCTIC ICE, 



are nothing more than those parts which stood between the 

 streams. Such as are aground, or have been so on rocks, 

 are easily known by having a regular tide mark on them, 

 and, for fear of latent danger, they are to be avoided. 

 The ice bergs met in Hudson's Straits and Bays descend 

 from the ice continent above the Linna^an Isles. Those 

 m^t with in the Atlantic come from Spitzbergen. 



