Geomorphology of Ulu Peninsula, James Ross Island, Antarctica
This study presents a 1:25,000 geomorphological map of the northern sector of Ulu Peninsula, James Ross Island, Antarctic Peninsula. The map covers an area of c. 250 km2, and documents the landforms and surficial sediments of one of the largest ice-free areas in Antarctica, based on remote sensing a...
| 发表在: | Journal of Maps |
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| Main Authors: | , , , , , , , , |
| 格式: | 文件 |
| 语言: | 英语 |
| 出版: |
Taylor & Francis Group
2021-12-01
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| 主题: | |
| 在线阅读: | http://dx.doi.org/10.1080/17445647.2021.1893232 |
| _version_ | 1856918476471402496 |
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| author | Stephen J. A. Jennings Bethan J. Davies Daniel Nývlt Neil F. Glasser Zbyněk Engel Filip Hrbáček Jonathan L. Carrivick Bedřich Mlčoch Michael J. Hambrey |
| author_facet | Stephen J. A. Jennings Bethan J. Davies Daniel Nývlt Neil F. Glasser Zbyněk Engel Filip Hrbáček Jonathan L. Carrivick Bedřich Mlčoch Michael J. Hambrey |
| author_sort | Stephen J. A. Jennings |
| collection | DOAJ |
| container_title | Journal of Maps |
| description | This study presents a 1:25,000 geomorphological map of the northern sector of Ulu Peninsula, James Ross Island, Antarctic Peninsula. The map covers an area of c. 250 km2, and documents the landforms and surficial sediments of one of the largest ice-free areas in Antarctica, based on remote sensing and field-based mapping. The large-scale landscape features are determined by the underlying Cretaceous sedimentary and Neogene volcanic geology, which has been sculpted by overlying ice masses during glacial periods. Paraglacial and periglacial features are superimposed upon remnant glacial features, reflecting the post-glacial evolution of the landscape. The study area can be broadly separated into three geomorphological sectors, according to the dominant contemporary Earth-surface processes; specifically, a glacierised southern sector, a paraglacial-dominated eastern sector, and a periglacial-dominated central/northern sector. This map provides a basis for further interdisciplinary research, and insight into the potential future landscape evolution of other parts of the Antarctic Peninsula as the climate warms. |
| format | Article |
| id | doaj-art-d64bf174a8d140fb8a3c8bf4f273cd2d |
| institution | Directory of Open Access Journals |
| issn | 1744-5647 |
| language | English |
| publishDate | 2021-12-01 |
| publisher | Taylor & Francis Group |
| record_format | Article |
| spelling | doaj-art-d64bf174a8d140fb8a3c8bf4f273cd2d2025-08-19T20:18:26ZengTaylor & Francis GroupJournal of Maps1744-56472021-12-0117212513910.1080/17445647.2021.18932321893232Geomorphology of Ulu Peninsula, James Ross Island, AntarcticaStephen J. A. Jennings0Bethan J. Davies1Daniel Nývlt2Neil F. Glasser3Zbyněk Engel4Filip Hrbáček5Jonathan L. Carrivick6Bedřich Mlčoch7Michael J. Hambrey8Masaryk UniversityRoyal Holloway University of LondonMasaryk UniversityAberystwyth UniversityFaculty of Science, Charles UniversityMasaryk UniversityUniversity of LeedsCzech Geological SurveyAberystwyth UniversityThis study presents a 1:25,000 geomorphological map of the northern sector of Ulu Peninsula, James Ross Island, Antarctic Peninsula. The map covers an area of c. 250 km2, and documents the landforms and surficial sediments of one of the largest ice-free areas in Antarctica, based on remote sensing and field-based mapping. The large-scale landscape features are determined by the underlying Cretaceous sedimentary and Neogene volcanic geology, which has been sculpted by overlying ice masses during glacial periods. Paraglacial and periglacial features are superimposed upon remnant glacial features, reflecting the post-glacial evolution of the landscape. The study area can be broadly separated into three geomorphological sectors, according to the dominant contemporary Earth-surface processes; specifically, a glacierised southern sector, a paraglacial-dominated eastern sector, and a periglacial-dominated central/northern sector. This map provides a basis for further interdisciplinary research, and insight into the potential future landscape evolution of other parts of the Antarctic Peninsula as the climate warms.http://dx.doi.org/10.1080/17445647.2021.1893232geomorphologypalaeoglaciologyulu peninsulajames ross islandantarctic peninsulaantarctica |
| spellingShingle | Stephen J. A. Jennings Bethan J. Davies Daniel Nývlt Neil F. Glasser Zbyněk Engel Filip Hrbáček Jonathan L. Carrivick Bedřich Mlčoch Michael J. Hambrey Geomorphology of Ulu Peninsula, James Ross Island, Antarctica geomorphology palaeoglaciology ulu peninsula james ross island antarctic peninsula antarctica |
| title | Geomorphology of Ulu Peninsula, James Ross Island, Antarctica |
| title_full | Geomorphology of Ulu Peninsula, James Ross Island, Antarctica |
| title_fullStr | Geomorphology of Ulu Peninsula, James Ross Island, Antarctica |
| title_full_unstemmed | Geomorphology of Ulu Peninsula, James Ross Island, Antarctica |
| title_short | Geomorphology of Ulu Peninsula, James Ross Island, Antarctica |
| title_sort | geomorphology of ulu peninsula james ross island antarctica |
| topic | geomorphology palaeoglaciology ulu peninsula james ross island antarctic peninsula antarctica |
| url | http://dx.doi.org/10.1080/17445647.2021.1893232 |
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