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Valley network morphology in the greater Meridiani Planum region, Mars

The Greater Meridiani Planum region on Mars is a key locale for a diverse range of fluvial landforms. Valley networks in this region have a range of geomorphologic styles that include negative relief, positive relief, or some combination of both along their lengths. Using high-resolution ~5–6 m/pixe...

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Detalles Bibliográficos
Autores principales: Chuang, Frank C., Williams, Rebecca M. E.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: 2018
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8549781/
https://www.ncbi.nlm.nih.gov/pubmed/34712355
http://dx.doi.org/10.1080/17445647.2018.1530154
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author Chuang, Frank C.
Williams, Rebecca M. E.
author_facet Chuang, Frank C.
Williams, Rebecca M. E.
author_sort Chuang, Frank C.
collection PubMed
description The Greater Meridiani Planum region on Mars is a key locale for a diverse range of fluvial landforms. Valley networks in this region have a range of geomorphologic styles that include negative relief, positive relief, or some combination of both along their lengths. Using high-resolution ~5–6 m/pixel orbital images in ArcGIS Desktop software, we mapped previously under-recognized fine-scale valley networks within the Greater Meridiani Planum region and recorded their geomorphic characteristics as feature attributes. The objectives in using the mapped features are to 1) document the full range of valley network morphologic types in the region, 2) document changes in morphologic types both on a regional scale and along the valley network segments, and 3) to use the mapped features along with other geologic information from previous studies to better understand landscape evolution in the Greater Meridiani Planum region.
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spelling pubmed-85497812021-10-27 Valley network morphology in the greater Meridiani Planum region, Mars Chuang, Frank C. Williams, Rebecca M. E. J Maps Article The Greater Meridiani Planum region on Mars is a key locale for a diverse range of fluvial landforms. Valley networks in this region have a range of geomorphologic styles that include negative relief, positive relief, or some combination of both along their lengths. Using high-resolution ~5–6 m/pixel orbital images in ArcGIS Desktop software, we mapped previously under-recognized fine-scale valley networks within the Greater Meridiani Planum region and recorded their geomorphic characteristics as feature attributes. The objectives in using the mapped features are to 1) document the full range of valley network morphologic types in the region, 2) document changes in morphologic types both on a regional scale and along the valley network segments, and 3) to use the mapped features along with other geologic information from previous studies to better understand landscape evolution in the Greater Meridiani Planum region. 2018-11-15 2018 /pmc/articles/PMC8549781/ /pubmed/34712355 http://dx.doi.org/10.1080/17445647.2018.1530154 Text en https://creativecommons.org/licenses/by/4.0/This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) ), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
spellingShingle Article
Chuang, Frank C.
Williams, Rebecca M. E.
Valley network morphology in the greater Meridiani Planum region, Mars
title Valley network morphology in the greater Meridiani Planum region, Mars
title_full Valley network morphology in the greater Meridiani Planum region, Mars
title_fullStr Valley network morphology in the greater Meridiani Planum region, Mars
title_full_unstemmed Valley network morphology in the greater Meridiani Planum region, Mars
title_short Valley network morphology in the greater Meridiani Planum region, Mars
title_sort valley network morphology in the greater meridiani planum region, mars
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8549781/
https://www.ncbi.nlm.nih.gov/pubmed/34712355
http://dx.doi.org/10.1080/17445647.2018.1530154
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