GEOLOGY OF THOUSAND ISLANDS. 91 



there, far inland, and high, above the sea, is 

 water-worn. 



4. Entire logs, with the roots on them, are 

 very rare either on the shore or inland. 



5. Many of these larger pieces bear marks of 

 the axe of ancient date.* 



6. Wherever drift-wood is found inland, or 

 above the level of the sea, it is generally 

 associated with the bones of whales ; so that I 

 think all these facts taken together make up a 

 pretty conclusive case against the in situ 

 suggestion. 



This island, as well as all the other off-lying 

 inlets and skerries on the south south-east and 

 south-west of Spitzbergen (I do not include 

 Hope Island), is composed of a rough coarse 

 grained trap rock, which in places imperfectly 

 assumes the columnar shape. These columns 

 seem very much shaken, as if ready to fall to 

 pieces, and the tops of the columns, as well as 

 all corners and protuberances, are much worn 

 and rounded, as if they had been half made 

 into boulders already. They, no doubt, are so, 

 for thousands of boulders, quite smooth and 

 rounded, and formed of the same rock, half 



* This might have been done since it came to Spitz 

 bergen, and so I do not lay much stress on this argument. 



