88 A JOURNEY IN BRAZIL. 



should now entertain the idea that the surface rocks are 

 everywhere decomposed, and that there is no erratic forma 

 tion or drift here. But upon close examination it is easy 

 to perceive that, while the decomposed rocks consist of 

 small particles of the primitive rocks which they represent, 

 with their dikes and all other characteristic features, there 

 is not a trace of larger or smaller boulders in them ; while 

 the superincumbent drift, consisting of a similar paste, 

 does not show the slightest sign of the indistinct stratifica 

 tion characteristic of the decomposed metamorphic rocks 

 below it, nor any of the decomposed dikes, but is full of 

 various kinds of boulders of various dimensions. I have 

 not yet traced the boulders to their origin ; but the majority 

 consist of a kind of greenstone composed of equal amounts 

 of a greenish black hornblende and feldspar. In Entre 

 Rios on the Parahyba, I was told by an engineer on the 

 road that in Minas Geraes iron mines are worked in a 

 rock like these boulders. This week I propose to explore 

 the Serra da Mantiqueira,* which separates the province 

 of Rio from Minas, and may advance the question further. 

 But you see that I need not go to the Andes to find 

 erratics, though it may yet be necessary for me to go, 

 in order to trace the evidence of glacier action in the 

 accumulation of this drift ; for you will notice that I 

 have only given you the evidence of extensive accumu 

 lations of drift similar in its characteristics to Northern 

 drift. But I have not yet seen a trace of glacial action 

 properly speaking, if polished surfaces and scratches and 

 furrows are especially to be considered as such. 



&quot;The decomposition of the surface rocks to the extent 

 to which it takes place here is very remarkable, and points 



* Mr. Agassiz was prevented from making this excursion. 



