332 USPALLATA PASS. [chap. xt. 



six thousand feet above tlie sea. This range has nearly the 

 same geographical position with respect to the Cordillera, which 

 the gigantic Portillo line has, but it is of a totally different 

 origin; it consists of various kinds of submarine lava, alternat- 

 ing with volcanic sandstones and other remarl^able sedimentary 

 deposits ; the whole having a very close resemblance to .some 

 of the tertiary beds on the shores of the Pacific. From tliis 

 resemblance I expected to find silicified wood, which is generally 

 characteristic of those formations. I was gratified in a very ex- 

 traordinary manner. In the central part of the range, at an 

 elevation of about seven thousand feet, I observed on a bare slope 

 some snow-white projecting columns. These were petrified 

 trees, eleven being silicified, and from thirty to forty converted 

 into coarsely-crystallized white calcareous spar. They were 

 abruptly broken off, the upright stumps projecting a few feet 

 above the ground. Tlie trunks measured from tiiree to five feet 

 each in circumference. They stood a little way apart from each 

 other, but the whole formed one group. Mr. Robert Brown has 

 been kind enough to examine the wood : he savs it belongs to the 

 fir tribe, partaking of the character of the Araucarian family, 

 but with some curious points of affinity with the yew. Tiio 

 volcanic sandstone in which the trees were embedded, and from 

 the lower part of which they must have sprung, had accumulated 

 in successive thin layers around their trunks ; and the stone yet 

 retained the impression of the bark. 



It required little geological practice to interpret tlie marvel- 

 lous story which this scene at once unfolded ; though I confess 

 I was at first so much astonished, that I could scarcely believe 

 the plainest evidence. I saw the spot where a cluster of fine 

 trees once waved their branches on the shores of the Atlantic, 

 when that ocean (now driven back 700 miles) came to the foot 

 of the Andes. I saw tiiat they had sprung from a volcanic soil 

 wiiich had been raised above the level of the sea, and that sub- 

 sequently this dry land, with its upright trees, had been let down 

 into the depths of the ocean. In these depths, the formerly dry 

 land was covered by sedimentary beds, and these again by 

 enormous streams of submarine lava — one such mass attainino: 

 the thickness of a thousand feet ; and these deluges of molten 

 stone and aqueous deposits five times alternately had been spread 



