420 A JOURNEY IN BRAZIL. 



denudation more extensive than any thus far recorded 

 in the annals of geology, which has given rise to all the 

 most prominent hills and mountain-chains along the north 

 ern bank of the river. Before seeking an explanation of 

 these facts, let us look at the third and uppermost deposit. 



This deposit is essentially the same as the Rio drift ; 

 but in the north it presents itself under a somewhat dif 

 ferent aspect. As in Rio, it is a clayey deposit, containing 

 more or less sand, and reddish in color, though varying 

 from deep ochre to a brownish tint. It is not so abso 

 lutely destitute of stratification here as in its more south 

 ern range, though the traces of stratification are rare, 

 and, when they do occur, are faint and indistinct. The 

 materials are also more completely comminuted, and, as I 

 said above, contain hardly any large masses, though quartz 

 pebbles are sometimes scattered throughout the deposit. 

 and occasionally a thin seam of pebbles, exactly as in the 

 Rio drift, is seen resting between it and the underlying 

 sandstone. In some places this bed of pebbles intersects 

 even the mass of the clay, giving it, in such instances, 

 an unquestionably stratified character. There can be no 

 doubt that this more recent formation rests unconform- 

 ably upon the sandstone beds beneath it ; for it fills all 

 the inequalities of their denudated surfaces, whether they 

 be more or less limited furrows, or wide, undulating de 

 pressions. It may be seen everywhere along the banks 

 of the river, above the stratified sandstone, sometimes 

 with the river-mud accumulated against it ; at the season 

 of the enchente, or high water, it is the only formation left 

 exposed above the water-level. Its thickness is not great ; 

 it varies from twenty or thirty to fifty feet, and may occa 

 sionally rise nearly to a hundred feet in height, though this 



