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2016 | OriginalPaper | Buchkapitel

1. The Urubamba in Panoptic Perspective

verfasst von : Daniel W. Gade

Erschienen in: Spell of the Urubamba

Verlag: Springer International Publishing

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Abstract

A far western tributary of the Amazon system, the Urubamba River has formed a main valley that anchors this discussion of Andean land and life. The valley floor at its southern point exceeds 4300 m asl; the valley ends below 300 m above sea level (asl) where the Urubamba joins the Tambo River to form the Ucayali. This 862 km-long depression manifests notable diversity of climate, vegetation and land use. In the temperate environment above 1800 m asl, human settlement and agriculture were important both before and after the Spanish Conquest (1532 ad). In contrast, the tropical environment in the Urubamba below 1800 m asl, except for a small periphery, had minimal Inca occupation. In the late sixteenth century, the Spaniards began to establish coca and sugar cane haciendas. Observational data and documents from the past introduce a diachronic understanding of the Urubamba as a valley region. Fieldwork beginning in 1963 validated that the place is wondrous in its ecologically diversity and traditional in its way of life, but also that it was on the cusp of change as land tenure became the major issue.

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Fußnoten
1
An English-language summary of Robledo’s paper delivered to the Sociedad Geográfica de Lima in January 1899 made foreigners who were interested in Peru aware of its importance. Luis Maria Robledo Ocampo, born on Hacienda Masapata in La Convención, became known in Cusco as an explorer and as an entrepreneur in Peru’s eastern region. He died in the revolution of 1910.
 
2
Cusco first received electricity in 1914 through the entrepreneurship of Cesar de Luchi Lomellini, an Italian immigrant, who financed a water-powered turbine and transmission line from it.
 
3
Atalaya is actually on the Rio Tambo about 1 km from its confluence with the Urubamba.
 
4
The Cordillera de Vilcanota and Cordillera de Urubamba, which begins north of Urcos, are sometimes considered as one chain.
 
5
Climatic understanding of the Urubamba suffers from incomplete and sometimes unreliable records. The only long-term and reliable station is outside the valley at Cusco (3400 m asl) where the average temperature is 12.8 °C and the coolest average monthly low temperature of −1 °C occurs in July. Cusco receives 707 mm, more rain than any place in the Upper Urubamba Valley.
 
6
All weather statistics in this chapter are from SENAMBI, the acronym for the Servicio Nacional de Meteorología e Hidrología del Perú, the entity responsible for generating weather and climate data for the country. Reliability of meteorological data in the valley remains problematical, due to the sparse network of stations in a zone of rapid temperature variations and questionable local records.
 
7
In Canas Province, Department of Cusco, six Indian communities, of which the largest is Quehue, have traditionally had the responsibility for remaking this bridge called Q’eswachaca over the Apurimac River. At an elevation of 3654 m above sea level, the natural vegetation is ichu grass (Stipa ichu), so the raw material for the bridge was also grass. Each community still contributes twined rope for its renovation even though, in the 1960s, a metal truss bridge was built a few meters from this site.
 
8
Statistics revealed that tourism in 2007 represented 27 % of the regional income and that the average foreign tourist spent US$987 compared to US$298 by Peruvian tourists. Of the 922, 487 tourists in Cusco in that year, 68.5 % were foreign and 31.5 % were domestic. Visitors spent an average of 3 days in Cusco including, for the great majority, a trip to Machu Picchu.
 
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Metadaten
Titel
The Urubamba in Panoptic Perspective
verfasst von
Daniel W. Gade
Copyright-Jahr
2016
DOI
https://doi.org/10.1007/978-3-319-20849-7_1