Syn-and post-glacial processes at the eastern slope of the Lanín volcano, Neuquén Province

The evolution of the Lanín volcano has been initially proposed from the basis of the study of its western slope. Field description of the deposits hosted in the eastern Argentinian slope has allowed improving the knowledge of this evolution. A reconstruction of the glacial and volcanic history of th...

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Detalles Bibliográficos
Autores principales:	Fennell, L.M., Ramos, M.E., Folguera, A.
Formato:	JOUR
Materias:	Apical caldera collapse Lanín volcano Patagonian Andes Volcanism avalanche caldera lahar pyroclastic flow volcanism Lanin Volcano Patagonia
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_00044822_v71_n1_p_Fennell
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

id	todo:paper_00044822_v71_n1_p_Fennell
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spelling	todo:paper_00044822_v71_n1_p_Fennell2023-10-03T13:59:03Z Syn-and post-glacial processes at the eastern slope of the Lanín volcano, Neuquén Province Fennell, L.M. Ramos, M.E. Folguera, A. Apical caldera collapse Lanín volcano Patagonian Andes Volcanism avalanche caldera lahar pyroclastic flow volcanism Lanin Volcano Patagonia The evolution of the Lanín volcano has been initially proposed from the basis of the study of its western slope. Field description of the deposits hosted in the eastern Argentinian slope has allowed improving the knowledge of this evolution. A reconstruction of the glacial and volcanic history of the area in recent times is carried out in this work which reveals the existence of large avalanches, lahars, lava flows and pyroclastic materials of syn- and post-glacial times. In particular, the interaction between these deposits and those deposited by the ice masses that covered the Lanín volcano allowed identifying two synglacial, one interglacial and two postglacial lava events. The postglacial history of this volcano involves voluminous avalanches related to a partial collapse of the cone summit part, and extensive surge-pyroclastic plains covering the surface of the volcanic edifice. Pyroclastic flows, lahars and pyroclastic monogenetic cones represent the most modern activity registered in the eastern slope of the Lanín volcano. Thus, since the study of the distribution of these sections, a more convulsed recent past than previously thought is revealed. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_00044822_v71_n1_p_Fennell
institution	Universidad de Buenos Aires
institution_str	I-28
repository_str	R-134
collection	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic	Apical caldera collapse Lanín volcano Patagonian Andes Volcanism avalanche caldera lahar pyroclastic flow volcanism Lanin Volcano Patagonia
spellingShingle	Apical caldera collapse Lanín volcano Patagonian Andes Volcanism avalanche caldera lahar pyroclastic flow volcanism Lanin Volcano Patagonia Fennell, L.M. Ramos, M.E. Folguera, A. Syn-and post-glacial processes at the eastern slope of the Lanín volcano, Neuquén Province
topic_facet	Apical caldera collapse Lanín volcano Patagonian Andes Volcanism avalanche caldera lahar pyroclastic flow volcanism Lanin Volcano Patagonia
description	The evolution of the Lanín volcano has been initially proposed from the basis of the study of its western slope. Field description of the deposits hosted in the eastern Argentinian slope has allowed improving the knowledge of this evolution. A reconstruction of the glacial and volcanic history of the area in recent times is carried out in this work which reveals the existence of large avalanches, lahars, lava flows and pyroclastic materials of syn- and post-glacial times. In particular, the interaction between these deposits and those deposited by the ice masses that covered the Lanín volcano allowed identifying two synglacial, one interglacial and two postglacial lava events. The postglacial history of this volcano involves voluminous avalanches related to a partial collapse of the cone summit part, and extensive surge-pyroclastic plains covering the surface of the volcanic edifice. Pyroclastic flows, lahars and pyroclastic monogenetic cones represent the most modern activity registered in the eastern slope of the Lanín volcano. Thus, since the study of the distribution of these sections, a more convulsed recent past than previously thought is revealed.
format	JOUR
author	Fennell, L.M. Ramos, M.E. Folguera, A.
author_facet	Fennell, L.M. Ramos, M.E. Folguera, A.
author_sort	Fennell, L.M.
title	Syn-and post-glacial processes at the eastern slope of the Lanín volcano, Neuquén Province
title_short	Syn-and post-glacial processes at the eastern slope of the Lanín volcano, Neuquén Province
title_full	Syn-and post-glacial processes at the eastern slope of the Lanín volcano, Neuquén Province
title_fullStr	Syn-and post-glacial processes at the eastern slope of the Lanín volcano, Neuquén Province
title_full_unstemmed	Syn-and post-glacial processes at the eastern slope of the Lanín volcano, Neuquén Province
title_sort	syn-and post-glacial processes at the eastern slope of the lanín volcano, neuquén province
url	http://hdl.handle.net/20.500.12110/paper_00044822_v71_n1_p_Fennell
work_keys_str_mv	AT fennelllm synandpostglacialprocessesattheeasternslopeofthelaninvolcanoneuquenprovince AT ramosme synandpostglacialprocessesattheeasternslopeofthelaninvolcanoneuquenprovince AT folgueraa synandpostglacialprocessesattheeasternslopeofthelaninvolcanoneuquenprovince
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Syn-and post-glacial processes at the eastern slope of the Lanín volcano, Neuquén Province

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