RECENT CHANGES IN GLACIERS AND PARAGLACIAL SYSTEMS, ANTARCTIC MARITIME
The article investigates changes in paraglacial systems and interconnections with glacial shrinkage on King George Island, Maritime Antarctica. The proglacial environment, as a result of recent deglaciation, was analyzed, and the types of landforms and at different scales were identified. These reco...
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Universidade Federal do Rio Grande do Norte
2020
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Online Access: | https://periodicos.ufrn.br/revistadoregne/article/view/19301 |
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ftunifrgnorteojs:oai:periodicos.ufrn.br:article/19301 2023-10-01T03:52:09+02:00 RECENT CHANGES IN GLACIERS AND PARAGLACIAL SYSTEMS, ANTARCTIC MARITIME RECIENTES CAMBIOS EN GLACIARES Y SISTEMAS PARAGLACIARES, ANTÁRTICA MARÍTIMA RECENTES ALTERAÇÕES NAS GELEIRAS E NOS SISTEMAS PARAGLACIAIS, ANTÁRTICA MARÍTIMA Perondi, Cleiva Rosa, Kátia Kellem da Petsch, Carina Idalino, Filipe Daros Oliveira, Manoela Araújo Gonçalves de Lorenz, Júlia Lopes Vieira, Rosemary Simões, Jefferson Cardia 2020-12-28 application/pdf https://periodicos.ufrn.br/revistadoregne/article/view/19301 por eng por eng Universidade Federal do Rio Grande do Norte https://periodicos.ufrn.br/revistadoregne/article/view/19301/13618 https://periodicos.ufrn.br/revistadoregne/article/view/19301/13619 https://periodicos.ufrn.br/revistadoregne/article/view/19301 Copyright (c) 2020 Revista de Geociências do Nordeste Notheast Geoscience Journal; Vol. 6 No. 2 (2020); 292-301 Revista de Geociências do Nordeste; v. 6 n. 2 (2020); 292-301 2447-3359 10.21680/2447-3359.2020v6n2 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2020 ftunifrgnorteojs https://doi.org/10.21680/2447-3359.2020v6n2 2023-09-03T06:52:49Z The article investigates changes in paraglacial systems and interconnections with glacial shrinkage on King George Island, Maritime Antarctica. The proglacial environment, as a result of recent deglaciation, was analyzed, and the types of landforms and at different scales were identified. These records are useful for successive evolutionary stages paraglacial system reconstruction. Glaciers and paraglacial systems showed rapid changes and new landscapes were detected on King George Island. Glaciers presented an important change between 2000 and 2018, where its classification has changed from marine-terminating to land-terminating glacier (no-marine). There are currently 21 glaciers land-terminating on King George Island (corresponding to 31% of the glaciers) and 11 are present in Admiralty Bay. 25% of these glaciers were marine in 2000. The new paraglacial environments (since 2000) has 1.7 km2 of the total area. Ecology, Wanda, Windy, Anna South and Baranowski Glaciers showed outwash plain, talus slopes and fluvial channels landforms in recent paraglacial system. Geomorphological mapping shows that paraglacial processes which differ between environments marginal to glacier ice are not standardized. El artículo investiga los cambios en los sistemas paraglaciares y las interconexiones con la retracción de los glaciares en la isla Rey Jorge, Antártica Marítima. Se analizó el ambiente proglacial, resultado de la deglaciación reciente, y se identificaron los tipos de formas de relieve en sus diferentes escalas. Estos registros son útiles para la reconstrucción de sucesivas etapas evolutivas en el sistema paraglacial. Los glaciares y los sistemas paraglaciares están evolucionando rápidamente y se están detectando nuevos paisajes en la isla Rey Jorge. Los glaciares mostraron un cambio importante entre 2000 y 2018, donde su clasificación cambió de glaciar de terminación marina a glaciar de terminación terrestre (no marino). Actualmente hay 21 glaciares de terminación terrestres en la isla Rey Jorge (que corresponden ... Article in Journal/Newspaper Antarc* Antarctic Antarctica Antártica King George Island Portal de Periódicos Eletrônicos da UFRN (Universidade Federal do Rio Grande do Norte) Admiralty Bay Antarctic Isla Rey Jorge ENVELOPE(-58.250,-58.250,-62.050,-62.050) King George Island Rey Jorge ENVELOPE(-58.050,-58.050,-62.083,-62.083) Revista de Geociências do Nordeste 6 2 292 301 |
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Open Polar |
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Portal de Periódicos Eletrônicos da UFRN (Universidade Federal do Rio Grande do Norte) |
op_collection_id |
ftunifrgnorteojs |
language |
Portuguese English |
description |
The article investigates changes in paraglacial systems and interconnections with glacial shrinkage on King George Island, Maritime Antarctica. The proglacial environment, as a result of recent deglaciation, was analyzed, and the types of landforms and at different scales were identified. These records are useful for successive evolutionary stages paraglacial system reconstruction. Glaciers and paraglacial systems showed rapid changes and new landscapes were detected on King George Island. Glaciers presented an important change between 2000 and 2018, where its classification has changed from marine-terminating to land-terminating glacier (no-marine). There are currently 21 glaciers land-terminating on King George Island (corresponding to 31% of the glaciers) and 11 are present in Admiralty Bay. 25% of these glaciers were marine in 2000. The new paraglacial environments (since 2000) has 1.7 km2 of the total area. Ecology, Wanda, Windy, Anna South and Baranowski Glaciers showed outwash plain, talus slopes and fluvial channels landforms in recent paraglacial system. Geomorphological mapping shows that paraglacial processes which differ between environments marginal to glacier ice are not standardized. El artículo investiga los cambios en los sistemas paraglaciares y las interconexiones con la retracción de los glaciares en la isla Rey Jorge, Antártica Marítima. Se analizó el ambiente proglacial, resultado de la deglaciación reciente, y se identificaron los tipos de formas de relieve en sus diferentes escalas. Estos registros son útiles para la reconstrucción de sucesivas etapas evolutivas en el sistema paraglacial. Los glaciares y los sistemas paraglaciares están evolucionando rápidamente y se están detectando nuevos paisajes en la isla Rey Jorge. Los glaciares mostraron un cambio importante entre 2000 y 2018, donde su clasificación cambió de glaciar de terminación marina a glaciar de terminación terrestre (no marino). Actualmente hay 21 glaciares de terminación terrestres en la isla Rey Jorge (que corresponden ... |
format |
Article in Journal/Newspaper |
author |
Perondi, Cleiva Rosa, Kátia Kellem da Petsch, Carina Idalino, Filipe Daros Oliveira, Manoela Araújo Gonçalves de Lorenz, Júlia Lopes Vieira, Rosemary Simões, Jefferson Cardia |
spellingShingle |
Perondi, Cleiva Rosa, Kátia Kellem da Petsch, Carina Idalino, Filipe Daros Oliveira, Manoela Araújo Gonçalves de Lorenz, Júlia Lopes Vieira, Rosemary Simões, Jefferson Cardia RECENT CHANGES IN GLACIERS AND PARAGLACIAL SYSTEMS, ANTARCTIC MARITIME |
author_facet |
Perondi, Cleiva Rosa, Kátia Kellem da Petsch, Carina Idalino, Filipe Daros Oliveira, Manoela Araújo Gonçalves de Lorenz, Júlia Lopes Vieira, Rosemary Simões, Jefferson Cardia |
author_sort |
Perondi, Cleiva |
title |
RECENT CHANGES IN GLACIERS AND PARAGLACIAL SYSTEMS, ANTARCTIC MARITIME |
title_short |
RECENT CHANGES IN GLACIERS AND PARAGLACIAL SYSTEMS, ANTARCTIC MARITIME |
title_full |
RECENT CHANGES IN GLACIERS AND PARAGLACIAL SYSTEMS, ANTARCTIC MARITIME |
title_fullStr |
RECENT CHANGES IN GLACIERS AND PARAGLACIAL SYSTEMS, ANTARCTIC MARITIME |
title_full_unstemmed |
RECENT CHANGES IN GLACIERS AND PARAGLACIAL SYSTEMS, ANTARCTIC MARITIME |
title_sort |
recent changes in glaciers and paraglacial systems, antarctic maritime |
publisher |
Universidade Federal do Rio Grande do Norte |
publishDate |
2020 |
url |
https://periodicos.ufrn.br/revistadoregne/article/view/19301 |
long_lat |
ENVELOPE(-58.250,-58.250,-62.050,-62.050) ENVELOPE(-58.050,-58.050,-62.083,-62.083) |
geographic |
Admiralty Bay Antarctic Isla Rey Jorge King George Island Rey Jorge |
geographic_facet |
Admiralty Bay Antarctic Isla Rey Jorge King George Island Rey Jorge |
genre |
Antarc* Antarctic Antarctica Antártica King George Island |
genre_facet |
Antarc* Antarctic Antarctica Antártica King George Island |
op_source |
Notheast Geoscience Journal; Vol. 6 No. 2 (2020); 292-301 Revista de Geociências do Nordeste; v. 6 n. 2 (2020); 292-301 2447-3359 10.21680/2447-3359.2020v6n2 |
op_relation |
https://periodicos.ufrn.br/revistadoregne/article/view/19301/13618 https://periodicos.ufrn.br/revistadoregne/article/view/19301/13619 https://periodicos.ufrn.br/revistadoregne/article/view/19301 |
op_rights |
Copyright (c) 2020 Revista de Geociências do Nordeste |
op_doi |
https://doi.org/10.21680/2447-3359.2020v6n2 |
container_title |
Revista de Geociências do Nordeste |
container_volume |
6 |
container_issue |
2 |
container_start_page |
292 |
op_container_end_page |
301 |
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1778517864626520064 |