991 resultados para Cuzco Region (Peru)


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This layer is a georeferenced raster image of the historic paper map entitled: Lago Titicaca : plano formado sobre los trabajos de Pentland, Raimondi, Agassiz, etc. : para la conferencia que en la noche del 21 de Diciembre del ano de 1891, dio en el l'oeal de la Sociedad Geografica, el Dr. Dn. Ignacio La Puenta sobre el estudio monografico del Lago, bajo su aspecto fisico e historico, por Rafael E. Baluarte, cartografo de la Sociedad Geografica de Lima, Colaborador y dibujante del Mapa oficial del Peru del Profesor Sor A. Raimondi. It was published by Sociedad Geografica de Lima in 1893. Scale 1:500,000. Map in Spanish. The image inside the map neatline is georeferenced to the surface of the earth and fit to the 'Mercator' projection. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as drainage, cities and other human settlements, roads, railroads, and more. Relief is shown by hachures and spot heights. This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection and the Harvard University Library as part of the Open Collections Program at Harvard University project: Organizing Our World: Sponsored Exploration and Scientific Discovery in the Modern Age. Maps selected for the project correspond to various expeditions and represent a range of regions, originators, ground condition dates, scales, and purposes.

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"RME-4584; Geology and Mineralogy (TID-4500, 43rd Ed.).

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Ce mémoire de maîtrise a pour objectif de montrer la construction de la représentation visuelle de « l’indigène » de la région de Cuzco et sa relation avec le discours de « l’authenticité » tel que défini par l’indigénisme, l’anthropologie et le tourisme. Il s’intéresse au rôle que jouent les médias visuels et audiovisuels dans la création d’une image de l’indigène perçu comme « authentique » et d’un discours commun sur les Andes. Les documents visuels étudiés, tous produits par des Péruviens, sont une sélection de photographies prises par Martin Chambi entre 1920-1945, le film Kukuli (1961) coréalisé par les Cuzquéniens Luis Figueroa, Eulogio Nishiyama et César Villanueva et la publicité touristique de PromPerú, intitulée «Perú: Vive la leyenda» («Pérou : Vis la légende») (2008). Cette analyse fait ressortir la représentation folklorique et anthropologique de l’indigène telle que suggérée par ces documents, qui l’associent principalement avec les origines, la tradition et le passé précolombien. Elle démontre aussi comment les images constituent une alternative à la stratégie représentationnelle proposée par l’indigénisme lettré et offrent un autre regard sur la réalité. Ainsi, les images technologiques montrent des détails qui ne concordent pas avec les stéréotypes culturels et révèlent un monde d’identités plus nuancées. D’autre part, elles créent aussi un espace de collaboration –entre le photographe/cinéaste et leurs modèles– qui permet aux acteurs sociaux marginalisés de participer à leur propre représentation. Enfin, notre recherche établit le lien entre cette image de l’indigène andin et la promotion touristique du Pérou.

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The Yanque nonsulfide Pb-Zn deposit (inferred resources 12.5 Mt @ 3.7% Pb and @ 3.5% Zn) is located in the Andahuaylas-Yauri ore province (Cuzco, southern Peru). The deposit occurs within a base metal mineralized district, centered on the medium-sized Dolores porphyry copper. A thorough geological, mineralogical and geochemical study has carried out in order to define: the relationships between the Dolores Cu-porphyry ore and the Yanque Zn-Pb polymetallic mineralization, and the characteristics of the economic nonsulfide concentrations. Both sedimentary and igneous rocks constitute the backbone of the Yanque-Dolores area. The sedimentary lithologies belong to the Soraya, Mara and Ferrobamba Fms. (upper Jurassic-middle Cretaceous). The Yanque orebody is hosted by the Mara Fm., which prevailingly consists of a siliciclastic sedimentary breccia. The original sulfide mineralization consisted of galena, pyrite and sphalerite. The host rock has been affected by a strong hydrothermal alteration, characterized by prevailing sericite/illite, as in the typical porphyry-related phyllic-argillic alteration stage, and by minor kaolinite, dolomite and quartz. Minor element geochemistry, characterized by Sb, As, Mn, Ag and locally also by Cu, points to magmatic-hydrothermal related mineralizing fluids. The Pb isotopic compositions from Dolores and Yanque sulfides are similar, and are typical of the Tertiary magmatically-derived ores in this part of Peru. The hydrothermally altered rocks at Yanque have the same Pb isotopic compositions as the sulfides, thus confirming the hypothesis that the Yanque primary Zn-Pb mineralization may have been produced by hydrothermal circulation related to the emplacement of the Dolores Cu-porphyry, as it is the case of other porphyry Cu systems associated with polymetallic mineralization elsewhere. However, no simple genetic model for the mineralization involving just one fluid circulation episode is able to explain the data. The Yanque economic nonsulfide ore association consists of sauconite, hemimorphite, smithsonite and cerussite, which result from the weathering and alteration of the original sulfide mineralization. Zinc is allocated mainly in sauconite (Zn-smectite), rather than in carbonates: a factor strictly related to the prevailing siliciclastic character of the host rock. Distinctive features of the Yanque orebody are the comparable ore grades for both Pb and Zn (3.5% Zn and 3.7% Pb), and the inverse supergene chemical zoning. In fact, contrary to other supergene ores of this type, zinc prevails in the top zone of the Yanque deposit, whereas lead content increases with depth. Considering the different mobility of the two metals in solution, it may be assumed that most of the primary zinc that was the source for the Yanque nonsulfides was originally located far from the position occupied by the galena mineralization, whose remnants have been observed on site. Zinc sulfides may have been originally contained in the eroded rock volumes that surrounded the actual deposit: the zinc-rich solutions have possibly migrated through the siliciclastic Mara Fm. and precipitated the nonsulfide minerals by porosity filling and replacement processes. In this sense, the Yanque secondary Zn-Pb deposit could be considered as a special type of “Exotic” mineralization.

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En la Región la Libertad, la mayor producción pesquera artesanal descansa en tres pesquerías del ámbito costero: cangrejo violáceo, caracol negro y pulpo. La pesca de altura de la pota, es importante por los volúmenes que aporta a la pesquería. La evaluación, se realizó en el litoral de la Región La Libertad, desde Chérrepe (7°9’35,4”S – 79°41’8,2”W) hasta isla Corcovado (8°56’25,8”S - 78°41’49,4”W), del 8 al 28 de octubre 2012. El trabajo se efectuó en dos etapas: 16 días por mar y 5 días por mar somero, y comprendió los diversos tipos de muestreos en las estaciones, tanto biológicas como oceanográficas. El estudio se efectuó en treinta y nueve bancos de invertebrados marinos: siete de caracol negro, cuatro de pulpo, dos de concha de abanico, dos de almeja, dos de muy muy, cuatro de pepino de mar, y dieciocho de cangrejo violáceo.

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La evaluación de los bancos naturales, se realizó entre 07°10’27”S, 79°41’18”W (Punta Chérrepe) y 08°45’44,9”S, 78°47’42,2”W (Isla Chao), del 13 al 24 de diciembre 2011. Se evaluó ocho especies de invertebrados de importancia comercial en 15 bancos naturales. Las especies fueron: Platyxanthus orbignyi cangrejo violáceo, Stramonita chocolata caracol negro, Octopus mimus pulpo, Argopecten purpuratus concha de abanico, Semele sp. almeja, Emerita analoga muy muy, Pattalus molli pepino de mar, Donax sp. palabritas.

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"October 1957."

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ENGLISH: A study has been made of the distributions of the 28 species of Chaetognatha in the waters off Peru and southern Ecuador, based primarily on data from oceanographic surveys carried out between 1958 and 1961 by the Inter-American Tropical Tuna Commission, Scripps Institution of Oceanography, and the Institute of Marine Resources Research and Consejo de Investigaciones Hidrobiologicas of Peru. Data from expeditions previous to 1958 also were used to aid in the interpretation of these materials. SPANISH: Se ha realizado un estudio de la distribución de las 28 especies de quetognatos en las aguas frente al Perú y al Ecuador meridional, basado principalmente sobre datos de los reconocimientos oceanográficos efectuados entre 1958 y 1961 por la Comisión Interamericana del Atún Tropical, la Institución Scripps de Oceanografía, y por el Instituto de Investigación de los Recursos Marinos y el Consejo de Investigaciones Hidrobiológicas del Perú. También se emplearon datos de las expediciones anteriores a 1958 para ayudar a la interpretación de este material. (PDF contains 102 pages)

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ATP distribution in coastal waters off Peru was examined and was found to differ with hydrological conditions in this area; maximal values in the vicinity of an intense upwelling were the same in 1974 and 1978. ATP distribution was highly non-uniform in 1978, particularly in upper layers of the northern section, due to disruption of a community (dense patches of bloom), which began about 10-15 days before our observations, and also because of appearance of a red tide. Unusually intense microplankton metabolism was found in Peruvian waters, particularly in the lower layers of the northern section, where ATP concentration of 3.6 ?g/l were found. Values of live microplankton biomass presented.