440 A JOURNEY IN BRAZIL. 



glaciers, part to the icebergs and to freshets consequent on 

 their breaking up, they will find that they have covered 

 the whole ground, and that the two theories are perfectly 

 consistent with each other. I think the present disputes 

 upon this subject will end somewhat like those which di 

 vided the Neptunic and Plutonic schools of geologists in 

 the early part of this century ; the former of whom would 

 have it that all the rocks were due to the action of water, 

 the latter that they were wholly due to the action of fire. 

 The problem was solved, and harmony restored, when it 

 was found that both elements have been equally at work 

 in forming the solid crust of the globe. To the stranded 

 icebergs alluded to above, I have no doubt, is to be re 

 ferred the origin of the many lakes without outlets ex 

 isting all over the sandy tract along our coast, of which 

 Cape Cod forms a part. Not only the formation of these 

 lakes, but also that of our salt marshes and cranberry- 

 fields, I believe to be connected with the waning of the 

 ice period. 



I hope at some future time to publish in detail, with 

 the appropriate maps and illustrations, my observations 

 upon the changes of our coast, and other phenomena con 

 nected with the close of the glacial epoch in the United 

 States. To give results without an account of the investi 

 gations which have led to them, inverts the true method 

 of science ; and I should not have introduced the subject 

 here except to show that the fresh-water denudations and 

 the oceanic encroachments which have formed the Amazo 

 nian Valley, with its river system, are not isolated facts, 

 but that the process has been the same in both continents. 

 The extraordinary continuity and uniformity of the Ama 

 zonian deposits are due to the immense size of the basin 



