The origin of valleys crossing patagonia and their relation with cordilleran uplift

The infinite Patagonian steppe, its fluvial network and patterns of fiords and lakes is full of amazing uniqueness, their mere existence and beauty wake up our need of discovering their natural causes. This task requires to have been lost in the neverending Patagonia, to hold all of its infinite det...

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Autor principal: Ghiglione, Matias
Publicado: 2017
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Acceso en línea:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v74_n1_p102_Ghiglione
http://hdl.handle.net/20.500.12110/paper_00044822_v74_n1_p102_Ghiglione
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spelling paper:paper_00044822_v74_n1_p102_Ghiglione2023-06-08T14:26:52Z The origin of valleys crossing patagonia and their relation with cordilleran uplift Ghiglione, Matias Antecedent rivers Argentine shelf Atlantic ocean Magellan strait Pablo groeber Patagonia Cenozoic cordillera glacial erosion Gondwana mountain region terrain uplift valley Atlantic Ocean Beagle Channel Magellan Strait Patagonia The infinite Patagonian steppe, its fluvial network and patterns of fiords and lakes is full of amazing uniqueness, their mere existence and beauty wake up our need of discovering their natural causes. This task requires to have been lost in the neverending Patagonia, to hold all of its infinite details and contrasts and finally connect all the pieces of the puzzle together not leaving one bit behind, that was one of Pablo Groeber’s achievements. A capricious terrain characterize Patagonia, where some of the mountain valleys are below the level of extra-Andean Mesetas, and the northern lakes located in the eastern foothills drain towards the Pacific Ocean. The Southernmost Andes are affected by strong glacial erosion and traverse by the Magellan Strait and the Beagle Channel, allowing to navigate connecting both the Atlantic and Pacific oceans. The Andean rivers of Patagonia have to dodge the Somoncurá and Deseado massifs along the “codo del río Senguer”, a morphic feature inherited from Gondwana times, and shaped during the late Cenozoic. This history was evident for Groeber, who expressed the importance of rivers and glacial carving the Cordillera, a discussion that still is motive of debate, almost 100 years later. © 2017, Asociacion Geologica Argentina. All rights reserved. Fil:Ghiglione, M.C. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. 2017 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v74_n1_p102_Ghiglione http://hdl.handle.net/20.500.12110/paper_00044822_v74_n1_p102_Ghiglione
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Antecedent rivers
Argentine shelf
Atlantic ocean
Magellan strait
Pablo groeber
Patagonia
Cenozoic
cordillera
glacial erosion
Gondwana
mountain region
terrain
uplift
valley
Atlantic Ocean
Beagle Channel
Magellan Strait
Patagonia
spellingShingle Antecedent rivers
Argentine shelf
Atlantic ocean
Magellan strait
Pablo groeber
Patagonia
Cenozoic
cordillera
glacial erosion
Gondwana
mountain region
terrain
uplift
valley
Atlantic Ocean
Beagle Channel
Magellan Strait
Patagonia
Ghiglione, Matias
The origin of valleys crossing patagonia and their relation with cordilleran uplift
topic_facet Antecedent rivers
Argentine shelf
Atlantic ocean
Magellan strait
Pablo groeber
Patagonia
Cenozoic
cordillera
glacial erosion
Gondwana
mountain region
terrain
uplift
valley
Atlantic Ocean
Beagle Channel
Magellan Strait
Patagonia
description The infinite Patagonian steppe, its fluvial network and patterns of fiords and lakes is full of amazing uniqueness, their mere existence and beauty wake up our need of discovering their natural causes. This task requires to have been lost in the neverending Patagonia, to hold all of its infinite details and contrasts and finally connect all the pieces of the puzzle together not leaving one bit behind, that was one of Pablo Groeber’s achievements. A capricious terrain characterize Patagonia, where some of the mountain valleys are below the level of extra-Andean Mesetas, and the northern lakes located in the eastern foothills drain towards the Pacific Ocean. The Southernmost Andes are affected by strong glacial erosion and traverse by the Magellan Strait and the Beagle Channel, allowing to navigate connecting both the Atlantic and Pacific oceans. The Andean rivers of Patagonia have to dodge the Somoncurá and Deseado massifs along the “codo del río Senguer”, a morphic feature inherited from Gondwana times, and shaped during the late Cenozoic. This history was evident for Groeber, who expressed the importance of rivers and glacial carving the Cordillera, a discussion that still is motive of debate, almost 100 years later. © 2017, Asociacion Geologica Argentina. All rights reserved.
author Ghiglione, Matias
author_facet Ghiglione, Matias
author_sort Ghiglione, Matias
title The origin of valleys crossing patagonia and their relation with cordilleran uplift
title_short The origin of valleys crossing patagonia and their relation with cordilleran uplift
title_full The origin of valleys crossing patagonia and their relation with cordilleran uplift
title_fullStr The origin of valleys crossing patagonia and their relation with cordilleran uplift
title_full_unstemmed The origin of valleys crossing patagonia and their relation with cordilleran uplift
title_sort origin of valleys crossing patagonia and their relation with cordilleran uplift
publishDate 2017
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v74_n1_p102_Ghiglione
http://hdl.handle.net/20.500.12110/paper_00044822_v74_n1_p102_Ghiglione
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