La geología de Théodore Pavie

Pavie was born in Angers, France. He arrived to Montevideo in 1833. From there he went to Buenos Aires. He traversed the Pampa to Cordoba, San Luis and Mendoza. He crossed The Andes to Santiago de Chile, then went to Valparaiso and finally to Lima. He returned to Europe in 1834. He composed drawings...

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Autor principal: Ottone, Eduardo G.
Formato: Artículo revista
Lenguaje:Español
Publicado: Facultad de Ciencias Exactas, Físicas y Naturales 2020
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Acceso en línea:https://revistas.unc.edu.ar/index.php/FCEFyN/article/view/28655
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institution Universidad Nacional de Córdoba
institution_str I-10
repository_str R-10
container_title_str Revistas de la UNC
language Español
format Artículo revista
topic South America, explorers, 19th century, illustrations.
América del Sur, viajeros, siglo XIX, ilustraciones.
spellingShingle South America, explorers, 19th century, illustrations.
América del Sur, viajeros, siglo XIX, ilustraciones.
Ottone, Eduardo G.
La geología de Théodore Pavie
topic_facet South America, explorers, 19th century, illustrations.
América del Sur, viajeros, siglo XIX, ilustraciones.
author Ottone, Eduardo G.
author_facet Ottone, Eduardo G.
author_sort Ottone, Eduardo G.
title La geología de Théodore Pavie
title_short La geología de Théodore Pavie
title_full La geología de Théodore Pavie
title_fullStr La geología de Théodore Pavie
title_full_unstemmed La geología de Théodore Pavie
title_sort la geología de théodore pavie
description Pavie was born in Angers, France. He arrived to Montevideo in 1833. From there he went to Buenos Aires. He traversed the Pampa to Cordoba, San Luis and Mendoza. He crossed The Andes to Santiago de Chile, then went to Valparaiso and finally to Lima. He returned to Europe in 1834. He composed drawings of the Cerro de Montevideo, the coast of the La Plata estuary in Buenos Aires showing its terraced levels, and a view of the mouth of the Riachuelo with the La Punta Island, a geoform that does not exist today. He also made several compositions on the Sierras Pampeanas and, specially, on his trip across The Andes by the Uspallata Pass. His account of the crossing of this mountain range constantly referred to the weather stiffness of the last days of that winter. Pavie’s observations matches well with the historical series of the Mendoza River runoff which indicate that the spring of 1833 and the summer of 1834 was a period of high flow, normally related to the presence of abundant snow. Illustrations of Chile and Peru landscapes complete the compositions.
publisher Facultad de Ciencias Exactas, Físicas y Naturales
publishDate 2020
url https://revistas.unc.edu.ar/index.php/FCEFyN/article/view/28655
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