Travels in Peru and India: While Superintending the Collection of Chinchona Plants and Seeds in South America, and Their Introduction into India.Markham, Clements R. (Clements Robert), Sir
History
Travels in Peru and India: While Superintending the Collection of Chinchona Plants and Seeds in South America, and Their Introduction into India.
Markham, Clements R. (Clements Robert), Sir
Cinchona; India -- Description and travel; Peru -- Description and travel
But some of these villages are at greater distances from the foot
of the Andes than others; thus they are not in a straight line, and
the direct distance from Ollachea to the Bolivian frontier is a good
deal under 180 miles. The valleys in which the Caravaya villages are
situated are separated from each other by spurs of the Andes, many of
them so wild and precipitous as to be quite inaccessible; and there
is no means of passing from village to village, in many instances,
without crossing the Andes to Crucero or Macusani, and descending again
by another pass. For this reason Crucero, being in the most central
position, has been chosen as the site of the capital of the province,
though in a bleak and intensely cold region.
The geological formation of Caravaya is composed of non-fossiliferous
schists, micaceous and slightly ferruginous, with veins of quartz. It
is a portion of the extensive system of rocks which Mr. Forbes has
grouped together as belonging to the Silurian epoch, and which extends
almost continuously over an extent from north-west to south-east of
more than seven hundred miles, forming the mountain-chain of the
Eastern Andes, continuous from Cuzco, through Caravaya, to Bolivia.
These rocks throw off spurs along the eastern side of the main chain.
Of this formation, too, are the loftiest mountain-peaks in South
America:--Illampu, or Sorata (24,812 feet), and Illimani (24,155
feet). Illampu, Mr. Forbes assures us, is fossiliferous up to its very
summit.[307]
Such is a brief account of the geography of Caravaya, and especially
of the streams which combine to form the great river Purus, from the
rivers of the Paucartambo valley on the extreme north-west, to the
Pablo-bamba on the frontier of Bolivia. The streams flowing from the
Eastern Andes to the north-west of the Paucartambo system combine to
swell the Ucayali, while those to the south-east of the Pablo-bamba
fall into the Beni, one of the chief tributaries of the Madeira. The
intermediate streams are the sources of the unknown Purus, they are
all more or less auriferous, they flow through forests abounding in
valuable products, and through countries of inexhaustible capabilities.
Yet the courses of very few of them have been explored to distances of
seventy miles from their sources, and the main stream of the Purus, one
of the principal affluents of the Amazon, may be said to be entirely
unknown to geographers.
CHAPTER XIII.
CARAVAYA.--THE VALLEY OF SANDIA.
Public-domain text, read in full here on John Shaqi.
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