Lena Rubensdotter , Ionut Cristi Nicu , Knut Stalsberg
{"title":"Complex geohazards at a high-priority Arctic cultural heritage site at Russekeila – Kapp Linné, Svalbard","authors":"Lena Rubensdotter , Ionut Cristi Nicu , Knut Stalsberg","doi":"10.1016/j.catena.2025.108935","DOIUrl":null,"url":null,"abstract":"<div><div>Geohazards are a global phenomenon, affecting both modern infrastructure and remnants from history. The extreme climate change occurring in Arctic Svalbard makes it one of the most environmentally sensitive areas for cultural heritage (CH) in the Northern Hemisphere. The physical landscapes, comprising mountain slopes, glacial, fluvial, and coastal processes, in conjunction with the permafrost setting, collectively constitute a complex set of conditions that present significant challenges to the conservation of CH. In this study, a combination of fieldwork and remote sensing methods is employed to map and gain an understanding of the geological, topographical, and geomorphological setting of a nationally high-priority Arctic CH site, Russekeila, situated at the mouth of the Linnéelva river on the west-central coast of Spitsbergen. It is demonstrated that a range of hazards, including fluvial, coastal and permafrost processes, both gradual and rapid, have the potential to impact this unique CH. The relative importance of the hazards is evaluated in terms of their present activity. The findings indicate that the rapid coastal migration of the river mouth directly erodes a bluff of marine sediment origin, leading to the destruction of CH. Furthermore, slow but continuous deformation by surface solifluction affects other parts of the CH site. The geomorphological mapping has also identified the presence of permafrost-dependent thaw slumps and thermo-erosion gullies near the CH. These processes are rapid when initiated, but the precise future initiation points are difficult to predict. The continued future warming of the permafrost and changes in hydro-climatic conditions may result in the activation and expansion of all these processes, thereby threatening an even greater proportion of the fragile CH at Russekeila. Integrated studies of this nature, which combine geomorphological mapping with the monitoring of processes and environmental conditions over time, represent a comprehensive approach to the assessment of potential hazards, thereby providing a solid foundation for the development of effective preservation strategies.</div></div>","PeriodicalId":9801,"journal":{"name":"Catena","volume":"254 ","pages":"Article 108935"},"PeriodicalIF":5.4000,"publicationDate":"2025-03-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Catena","FirstCategoryId":"97","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0341816225002371","RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
Complex geohazards at a high-priority Arctic cultural heritage site at Russekeila – Kapp Linné, Svalbard
Geohazards are a global phenomenon, affecting both modern infrastructure and remnants from history. The extreme climate change occurring in Arctic Svalbard makes it one of the most environmentally sensitive areas for cultural heritage (CH) in the Northern Hemisphere. The physical landscapes, comprising mountain slopes, glacial, fluvial, and coastal processes, in conjunction with the permafrost setting, collectively constitute a complex set of conditions that present significant challenges to the conservation of CH. In this study, a combination of fieldwork and remote sensing methods is employed to map and gain an understanding of the geological, topographical, and geomorphological setting of a nationally high-priority Arctic CH site, Russekeila, situated at the mouth of the Linnéelva river on the west-central coast of Spitsbergen. It is demonstrated that a range of hazards, including fluvial, coastal and permafrost processes, both gradual and rapid, have the potential to impact this unique CH. The relative importance of the hazards is evaluated in terms of their present activity. The findings indicate that the rapid coastal migration of the river mouth directly erodes a bluff of marine sediment origin, leading to the destruction of CH. Furthermore, slow but continuous deformation by surface solifluction affects other parts of the CH site. The geomorphological mapping has also identified the presence of permafrost-dependent thaw slumps and thermo-erosion gullies near the CH. These processes are rapid when initiated, but the precise future initiation points are difficult to predict. The continued future warming of the permafrost and changes in hydro-climatic conditions may result in the activation and expansion of all these processes, thereby threatening an even greater proportion of the fragile CH at Russekeila. Integrated studies of this nature, which combine geomorphological mapping with the monitoring of processes and environmental conditions over time, represent a comprehensive approach to the assessment of potential hazards, thereby providing a solid foundation for the development of effective preservation strategies.
期刊介绍:
Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment.
Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.