- We Left Yaquil, And Followed The Flat
Valley, Formed Like That Of Quillota, In Which The Rio
Tinderidica Flows.
Even at these few miles south of Santiago
the climate is much damper; in consequence there are fine
tracts of pasturage, which are not irrigated.
(20th.) We l
followed this valley till it expanded into a great plain, which
reaches from the sea to the mountains west of Rancagua.
We shortly lost all trees and even bushes; so that the
inhabitants are nearly as badly off for firewood as those in
the Pampas. Never having heard of these plains, I was much
surprised at meeting with such scenery in Chile. The plains
belong to more than one series of different elevations, and
they are traversed by broad flat-bottomed valleys; both of
which circumstances, as in Patagonia, bespeak the action of
the sea on gently rising land. In the steep cliffs bordering
these valleys, there are some large caves, which no doubt
were originally formed by the waves: one of these is celebrated
under the name of Cueva del Obispo; having formerly
been consecrated. During the day I felt very unwell, and
from that time till the end of October did not recover.
September 22nd. - We continued to pass over green plains
without a tree. The next day we arrived at a house near
Navedad, on the sea-coast, where a rich Haciendero gave us
lodgings. I stayed here the two ensuing days, and although
very unwell, managed to collect from the tertiary formation
some marine shells.
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