The colorado river flood of 1914: Groeber’s first geological contribution since his arrival in Argentina

It is analyzed the report made by Pablo Groeber a few months after the catastrophic collapse of the Carri Lauquén paleolake developed in 1914 in the Main Cordillera between Mendoza and Neuquén. He presented the topographic survey of the area occupied by the paleolake, analyzed the causes of its form...

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Autor principal: Ramos, V.A.
Formato: JOUR
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_00044822_v74_n1_p9_Ramos
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spelling todo:paper_00044822_v74_n1_p9_Ramos2023-10-03T13:59:17Z The colorado river flood of 1914: Groeber’s first geological contribution since his arrival in Argentina Ramos, V.A. Catastrophic collapse Colorado river Main andes Mendoza Natural dam Neuquén Outburst flood catastrophic event dam flood flooding headwater natural disaster topographic mapping Andes Argentina Barrancas River Colorado River [Argentina] Mendoza Neuquen It is analyzed the report made by Pablo Groeber a few months after the catastrophic collapse of the Carri Lauquén paleolake developed in 1914 in the Main Cordillera between Mendoza and Neuquén. He presented the topographic survey of the area occupied by the paleolake, analyzed the causes of its formation, and estimated the volume of water released during the disaster. This was the highest known flood of the Colorado River, reaching its waters through more than 1000 km to the Atlantic. Groeber discussed the reasons for its outburst and the sudden flood produced downstream. The results obtained are evaluated by specific works carried out in the region over the past one hundred years, and it is emphasized the validity of his conclusions on the genesis of the paleolake, the causes of its rupture, the volume of the flood produced and the processes involved. Supplementing Groeber’s observations on the headwaters of the Barrancas River, are discussed the disasters produced downstream by the outburst flood in the Colorado River valley. This allows recording the variations of the height of the flood peak, decreasing from 32 to 3 meters, and the slowdown of the speed from 20 to 11 km per hour from the natural dam collapse to almost its mouth in the Atlantic Ocean. The analysis confirms the validity of the reconstruction of the processes described by Groeber one hundred years ago, and once again highlights the capacity and knowledge of this young geologist recently arrived in Argentina in his first published work in our country. © 2017, Asociacion Geologica Argentina. All rights reserved. Fil:Ramos, V.A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_00044822_v74_n1_p9_Ramos
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Catastrophic collapse
Colorado river
Main andes
Mendoza
Natural dam
Neuquén
Outburst flood
catastrophic event
dam
flood
flooding
headwater
natural disaster
topographic mapping
Andes
Argentina
Barrancas River
Colorado River [Argentina]
Mendoza
Neuquen
spellingShingle Catastrophic collapse
Colorado river
Main andes
Mendoza
Natural dam
Neuquén
Outburst flood
catastrophic event
dam
flood
flooding
headwater
natural disaster
topographic mapping
Andes
Argentina
Barrancas River
Colorado River [Argentina]
Mendoza
Neuquen
Ramos, V.A.
The colorado river flood of 1914: Groeber’s first geological contribution since his arrival in Argentina
topic_facet Catastrophic collapse
Colorado river
Main andes
Mendoza
Natural dam
Neuquén
Outburst flood
catastrophic event
dam
flood
flooding
headwater
natural disaster
topographic mapping
Andes
Argentina
Barrancas River
Colorado River [Argentina]
Mendoza
Neuquen
description It is analyzed the report made by Pablo Groeber a few months after the catastrophic collapse of the Carri Lauquén paleolake developed in 1914 in the Main Cordillera between Mendoza and Neuquén. He presented the topographic survey of the area occupied by the paleolake, analyzed the causes of its formation, and estimated the volume of water released during the disaster. This was the highest known flood of the Colorado River, reaching its waters through more than 1000 km to the Atlantic. Groeber discussed the reasons for its outburst and the sudden flood produced downstream. The results obtained are evaluated by specific works carried out in the region over the past one hundred years, and it is emphasized the validity of his conclusions on the genesis of the paleolake, the causes of its rupture, the volume of the flood produced and the processes involved. Supplementing Groeber’s observations on the headwaters of the Barrancas River, are discussed the disasters produced downstream by the outburst flood in the Colorado River valley. This allows recording the variations of the height of the flood peak, decreasing from 32 to 3 meters, and the slowdown of the speed from 20 to 11 km per hour from the natural dam collapse to almost its mouth in the Atlantic Ocean. The analysis confirms the validity of the reconstruction of the processes described by Groeber one hundred years ago, and once again highlights the capacity and knowledge of this young geologist recently arrived in Argentina in his first published work in our country. © 2017, Asociacion Geologica Argentina. All rights reserved.
format JOUR
author Ramos, V.A.
author_facet Ramos, V.A.
author_sort Ramos, V.A.
title The colorado river flood of 1914: Groeber’s first geological contribution since his arrival in Argentina
title_short The colorado river flood of 1914: Groeber’s first geological contribution since his arrival in Argentina
title_full The colorado river flood of 1914: Groeber’s first geological contribution since his arrival in Argentina
title_fullStr The colorado river flood of 1914: Groeber’s first geological contribution since his arrival in Argentina
title_full_unstemmed The colorado river flood of 1914: Groeber’s first geological contribution since his arrival in Argentina
title_sort colorado river flood of 1914: groeber’s first geological contribution since his arrival in argentina
url http://hdl.handle.net/20.500.12110/paper_00044822_v74_n1_p9_Ramos
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