Industrial and commercial South AmericaPeck, Annie S. (Annie Smith)
History
Industrial and commercial South America
Peck, Annie S. (Annie Smith)
South America; South America -- Economic conditions -- 1918-
=The Central Cordillera= is the true divide, forming the continental
watershed. A single river, the Marañon, breaks through in its lower
northern part, while 20 coast streams rising in the Central cut the
Maritime range; the East Cordillera is fractured by six Peruvian
rivers, the Marañon, Huallaga, Perené, Mantaro, Apurimac, Vilcamayu,
and Paucartambo, all but the first being affluents of the Ucayali,
which some authorities call a tributary of the Marañon. Oftener these
two are said to unite to form the Amazon.
=The East Cordillera.= While the Central Cordillera is volcanic in
part, the East is of Silurian formation, older and non-volcanic except
at the edge of Lake Titicaca. The last, in Bolivia a splendid range,
is lower in Peru. It has the high plateau region on the west; east is
the Amazon Basin into which its spurs extend for varying distances. The
Central and Eastern Andes are connected by a transverse mountain knot
at Vilcanota, or Cuzco, while a similar knot occurs at Cerro de Pasco.
Farther north the Central Cordillera separates the valleys of the
Marañon and the Huallaga, while the eastern Andes is between the latter
and the Ucayali. The three ranges are clearly defined much of the way
in Peru, and back of Chimbote in the section including the Huailas
Valley there are four.
THE MONTAÑA
The third longitudinal division in Peru, the Trans-Andine, usually
referred to as the _montaña_, is the region of subtropical and tropical
forest. It is traversed by great rivers, largely navigable. Partly
in the sierra country are the Marañon, 600, and the Huallaga, 400
miles long, before their union; 150 miles beyond they are joined by
the Ucayali, a great river with a course of 600 miles, more navigable
than the other two. These three rivers with their affluents drain the
northern and the central part of Peru. The streams of the southern
portion are tributary to the Madre de Dios which flows into the Beni,
the latter uniting with the Mamoré to form the Madeira. The _montaña_
section, 800 miles from north to south, has a sub-tropical region on
the lower slopes of the Andes, the branches of which run out 60 or 80
miles towards the lowlands, and the tropical forests of the latter.
In the northern section a considerable district between the Huallaga
and the Ucayali rivers, traversed by the Andes, is composed of grassy
plains called the Pampa del Sacramento. Some of this northern region is
called the _montaña_, having its characteristics, although not east of
the East Cordillera.
CLIMATE
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