Can topographic features of debris cones (SW Spitsbergen) be geoindicators of environmental changes?

Evidence of recent geomorphic processes within debris cones, their spatial distribution and diversification on cones surface are interpreted in the context of contemporary slope morphogenesis. The detailed inventory of relief features on debris cones in the SW Spitsbergen revealed their great spatia...

Full description

Bibliographic Details
Published in:Polish Polar Research
Main Authors: Agnieszka Latocha-Wites, Krzysztof Parzóch
Format: Article in Journal/Newspaper
Language:English
Published: Polish Academy of Sciences 2023
Subjects:
Online Access:https://doi.org/10.24425/ppr.2023.144539
https://doaj.org/article/d16ff71ac35b42959d2665e906a2a898
id ftdoajarticles:oai:doaj.org/article:d16ff71ac35b42959d2665e906a2a898
record_format openpolar
spelling ftdoajarticles:oai:doaj.org/article:d16ff71ac35b42959d2665e906a2a898 2023-08-20T04:04:29+02:00 Can topographic features of debris cones (SW Spitsbergen) be geoindicators of environmental changes? Agnieszka Latocha-Wites Krzysztof Parzóch 2023-03-01T00:00:00Z https://doi.org/10.24425/ppr.2023.144539 https://doaj.org/article/d16ff71ac35b42959d2665e906a2a898 EN eng Polish Academy of Sciences https://journals.pan.pl/Content/126246/PDF/2023-03-PPR-05.pdf https://doaj.org/toc/0138-0338 0138-0338 https://doi.org/10.24425/ppr.2023.144539 https://doaj.org/article/d16ff71ac35b42959d2665e906a2a898 Polish Polar Research, Vol vol. 44, Iss No 3 : Special Issue to celebrate 50 years anniversary of Stanislaw Baranowski Polar Station in Spitsbergen: Part 2, Pp 291-312 (2023) arctic svalbard slope morphology geomorphic processes debris flow Geology QE1-996.5 article 2023 ftdoajarticles https://doi.org/10.24425/ppr.2023.144539 2023-07-30T00:38:10Z Evidence of recent geomorphic processes within debris cones, their spatial distribution and diversification on cones surface are interpreted in the context of contemporary slope morphogenesis. The detailed inventory of relief features on debris cones in the SW Spitsbergen revealed their great spatial diversity. It is linked with a dominance of different morphological processes in adjacent areas. Spatial and temporal diversity of process-relief assemblages on cones is strongly related with local factors, like bedrock lithology, slope aspect and inclination, local circulation and climatic conditions. However, the potential role of debris cones and their topographic features as geoindicators archiving information about the environmental impact of global changes, cannot be explicitly estimated. Local constraints obscure the regional expression of any global trends, which could be detected on the basis of process-relief assemblages on debris cones in polar regions. Article in Journal/Newspaper Arctic Polar Research Svalbard Spitsbergen Directory of Open Access Journals: DOAJ Articles Arctic Svalbard Polish Polar Research
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic arctic
svalbard
slope morphology
geomorphic processes
debris flow
Geology
QE1-996.5
spellingShingle arctic
svalbard
slope morphology
geomorphic processes
debris flow
Geology
QE1-996.5
Agnieszka Latocha-Wites
Krzysztof Parzóch
Can topographic features of debris cones (SW Spitsbergen) be geoindicators of environmental changes?
topic_facet arctic
svalbard
slope morphology
geomorphic processes
debris flow
Geology
QE1-996.5
description Evidence of recent geomorphic processes within debris cones, their spatial distribution and diversification on cones surface are interpreted in the context of contemporary slope morphogenesis. The detailed inventory of relief features on debris cones in the SW Spitsbergen revealed their great spatial diversity. It is linked with a dominance of different morphological processes in adjacent areas. Spatial and temporal diversity of process-relief assemblages on cones is strongly related with local factors, like bedrock lithology, slope aspect and inclination, local circulation and climatic conditions. However, the potential role of debris cones and their topographic features as geoindicators archiving information about the environmental impact of global changes, cannot be explicitly estimated. Local constraints obscure the regional expression of any global trends, which could be detected on the basis of process-relief assemblages on debris cones in polar regions.
format Article in Journal/Newspaper
author Agnieszka Latocha-Wites
Krzysztof Parzóch
author_facet Agnieszka Latocha-Wites
Krzysztof Parzóch
author_sort Agnieszka Latocha-Wites
title Can topographic features of debris cones (SW Spitsbergen) be geoindicators of environmental changes?
title_short Can topographic features of debris cones (SW Spitsbergen) be geoindicators of environmental changes?
title_full Can topographic features of debris cones (SW Spitsbergen) be geoindicators of environmental changes?
title_fullStr Can topographic features of debris cones (SW Spitsbergen) be geoindicators of environmental changes?
title_full_unstemmed Can topographic features of debris cones (SW Spitsbergen) be geoindicators of environmental changes?
title_sort can topographic features of debris cones (sw spitsbergen) be geoindicators of environmental changes?
publisher Polish Academy of Sciences
publishDate 2023
url https://doi.org/10.24425/ppr.2023.144539
https://doaj.org/article/d16ff71ac35b42959d2665e906a2a898
geographic Arctic
Svalbard
geographic_facet Arctic
Svalbard
genre Arctic
Polar Research
Svalbard
Spitsbergen
genre_facet Arctic
Polar Research
Svalbard
Spitsbergen
op_source Polish Polar Research, Vol vol. 44, Iss No 3 : Special Issue to celebrate 50 years anniversary of Stanislaw Baranowski Polar Station in Spitsbergen: Part 2, Pp 291-312 (2023)
op_relation https://journals.pan.pl/Content/126246/PDF/2023-03-PPR-05.pdf
https://doaj.org/toc/0138-0338
0138-0338
https://doi.org/10.24425/ppr.2023.144539
https://doaj.org/article/d16ff71ac35b42959d2665e906a2a898
op_doi https://doi.org/10.24425/ppr.2023.144539
container_title Polish Polar Research
_version_ 1774714868923891712