250 A JOURNEY IN BRAZIL. 



observations on this subject. Although he has been al 

 most constantly occupied with his collections, he has, 

 nevertheless, found time to examine the geological for 

 mations of the neighborhood. The more he considers the 

 mazons and its tributaries, the more does he feel con 

 vinced that the whole mass of the reddish, homogene- 

 clay, which he has called drift, is the glacial de 

 posit brought down from the Andes and worked over by 

 the melting of the ice which transported it. According 

 to his view, the whole valley was originally filled with 

 this deposit, and the Amazons itself, as well as the rivers 

 connected with it, are so many channels worn through the 

 mass, having cut their way just as the igarap now wears 

 its way through the more modern deposits of mud and sand. 

 It may seem strange that any one should compare the for 

 mation of these insignificant forest-streams with that of 

 the vast river which pours itself across a whole continent ; 

 but it is, after all, only a reversal of the microscopic process 

 of investigation. We magnify the microscopically small in 

 order to see it, and we must diminish that which transcends 

 our apprehension by its great size, in order to understand 

 it. The naturalist who wishes to compare an elephant with 

 a Coni (Hyrax),* turns the diminishing end of his glass 

 upon the former, and, reducing its clumsy proportions, he 

 finds that the difference is one of size rather than struc 

 ture. The essential features are the same. So the little 

 igarape, as it wears its channel through the forest to-day, 

 explains the early history of the great river and feebly 

 reiterates the past. 



* It was Cuvier who first ascertained that the small Hyrax belongs to the 

 same order as the elephant. 



