{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2025,12,3]],"date-time":"2025-12-03T18:04:52Z","timestamp":1764785092651,"version":"build-2065373602"},"reference-count":81,"publisher":"MDPI AG","issue":"6","license":[{"start":{"date-parts":[[2023,3,7]],"date-time":"2023-03-07T00:00:00Z","timestamp":1678147200000},"content-version":"vor","delay-in-days":0,"URL":"https:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"funder":[{"name":"Deutsche Forschungsgemeinschaft (DFG, German Research Foundation)","award":["BE 1118\/38-2","BE 1118\/39-2","BE 1118\/40-2","HA 5740\/10-2","I 4062"],"award-info":[{"award-number":["BE 1118\/38-2","BE 1118\/39-2","BE 1118\/40-2","HA 5740\/10-2","I 4062"]}]},{"DOI":"10.13039\/501100002428","name":"AustrianScience Fund (FWF)","doi-asserted-by":"publisher","award":["BE 1118\/38-2","BE 1118\/39-2","BE 1118\/40-2","HA 5740\/10-2","I 4062"],"award-info":[{"award-number":["BE 1118\/38-2","BE 1118\/39-2","BE 1118\/40-2","HA 5740\/10-2","I 4062"]}],"id":[{"id":"10.13039\/501100002428","id-type":"DOI","asserted-by":"publisher"}]}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Remote Sensing"],"abstract":"<jats:p>Deglaciation in high mountain areas signifies the transition from glacial to periglacial conditioned landscapes. Due to the reduced melt rate of debris-covered glacier ice, these areas of the glacier may persist long after the surrounding glacier has melted, resulting in the formation of distinct post-glacial landforms. In this study, we examine the geomorphological evolution and potential future development of a 19,267 m3 \u00b1 204 m3 rockfall from the permafrost-affected headwall on the low-elevated Zwieselbachferner in the Horlachtal, Stubai Alps, Austria. The analysis uses multi-epochal remote sensing data, including photogrammetrically and airborne laser scanning-derived digital elevation models, orthophotos, and satellite data, covering a period from the initial rockfall in 2003\/2004 to 2022. The data reveals that the rockfall event resulted in the formation of a supraglacial debris layer of varying thickness, spanning an area of 15,920 m2. Subsequently, 13 further rockfalls ranging from 67 m3 \u00b1 6 m3 to 4250 m3 \u00b1 121 m3 were detected. The mean ice thickness of the debris-covered area only slightly decreased between 2006 and 2022, in contrast to the surrounding glacier, whose thickness and length have strongly decreased. This results in the formation of a steep front and flanks that become increasingly covered by debris redistribution. The study suggests that the glacier ice covered by rockfall-derived debris will remain as a periglacial landform of glacial origin after the complete melting of the surrounding glacier.<\/jats:p>","DOI":"10.3390\/rs15061472","type":"journal-article","created":{"date-parts":[[2023,3,7]],"date-time":"2023-03-07T01:43:35Z","timestamp":1678153415000},"page":"1472","update-policy":"https:\/\/doi.org\/10.3390\/mdpi_crossmark_policy","source":"Crossref","is-referenced-by-count":4,"title":["Glaciogenic Periglacial Landform in the Making\u2014Geomorphological Evolution of a Rockfall on a Small Glacier in the Horlachtal, Stubai Alps, Austria"],"prefix":"10.3390","volume":"15","author":[{"given":"Fabian","family":"Fleischer","sequence":"first","affiliation":[{"name":"Department of Physical Geography, Catholic University of Eichst\u00e4tt-Ingolstadt, 95072 Eichst\u00e4tt, Germany"}]},{"given":"Florian","family":"Haas","sequence":"additional","affiliation":[{"name":"Department of Physical Geography, Catholic University of Eichst\u00e4tt-Ingolstadt, 95072 Eichst\u00e4tt, Germany"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-7880-7785","authenticated-orcid":false,"given":"Moritz","family":"Altmann","sequence":"additional","affiliation":[{"name":"Department of Physical Geography, Catholic University of Eichst\u00e4tt-Ingolstadt, 95072 Eichst\u00e4tt, Germany"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-0305-0375","authenticated-orcid":false,"given":"Jakob","family":"Rom","sequence":"additional","affiliation":[{"name":"Department of Physical Geography, Catholic University of Eichst\u00e4tt-Ingolstadt, 95072 Eichst\u00e4tt, Germany"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-3716-8961","authenticated-orcid":false,"given":"Camillo","family":"Ressl","sequence":"additional","affiliation":[{"name":"Department of Geodesy and Geoinformation, Technische Universit\u00e4t Wien, 1040 Vienna, Austria"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-9214-8165","authenticated-orcid":false,"given":"Michael","family":"Becht","sequence":"additional","affiliation":[{"name":"Department of Physical Geography, Catholic University of Eichst\u00e4tt-Ingolstadt, 95072 Eichst\u00e4tt, Germany"}]}],"member":"1968","published-online":{"date-parts":[[2023,3,7]]},"reference":[{"key":"ref_1","doi-asserted-by":"crossref","first-page":"726","DOI":"10.1038\/s41586-021-03436-z","article-title":"Accelerated global glacier mass loss in the early twenty-first century","volume":"592","author":"Hugonnet","year":"2021","journal-title":"Nature"},{"key":"ref_2","doi-asserted-by":"crossref","first-page":"382","DOI":"10.1038\/s41586-019-1071-0","article-title":"Global glacier mass changes and their contributions to sea-level rise from 1961 to 2016","volume":"568","author":"Zemp","year":"2019","journal-title":"Nature"},{"key":"ref_3","doi-asserted-by":"crossref","first-page":"753","DOI":"10.5194\/tc-9-753-2015","article-title":"Tracing glacier changes in Austria from the Little Ice Age to the present using a lidar-based high-resolution glacier inventory in Austria","volume":"9","author":"Fischer","year":"2015","journal-title":"Cryosphere"},{"key":"ref_4","doi-asserted-by":"crossref","first-page":"1125","DOI":"10.5194\/tc-13-1125-2019","article-title":"Modelling the future evolution of glaciers in the European Alps under the EURO-CORDEX RCM ensemble","volume":"13","author":"Zekollari","year":"2019","journal-title":"Cryosphere"},{"key":"ref_5","unstructured":"Ballantyne, C.K. 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