Surface morphological types and spatial distribution of fan-shaped landforms in the periglacial high-Arctic environment of central Spitsbergen, Svalbard

A 1:19,500 map of the Petunibukta region documents the spatial distribution of almost 300 colluvial and alluvial fans (together with their catchments) in the periglacial high-Arctic environment of Svalbard. Fan-shaped landforms were mapped using an orthophoto and digital elevation model generated fr...

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Main Authors: Aleksandra M. Tomczyk, Marek W. Ewertowski
Format: Article
Language:English
Published: Taylor & Francis Group 2017-11-01
Series:Journal of Maps
Subjects:
GIS
Online Access:http://dx.doi.org/10.1080/17445647.2017.1294543
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spelling doaj-15975e98f13d409084c337c7cbaa111b2020-11-25T01:31:57ZengTaylor & Francis GroupJournal of Maps1744-56472017-11-0113223925110.1080/17445647.2017.12945431294543Surface morphological types and spatial distribution of fan-shaped landforms in the periglacial high-Arctic environment of central Spitsbergen, SvalbardAleksandra M. Tomczyk0Marek W. Ewertowski1Adam Mickiewicz UniversityAdam Mickiewicz UniversityA 1:19,500 map of the Petunibukta region documents the spatial distribution of almost 300 colluvial and alluvial fans (together with their catchments) in the periglacial high-Arctic environment of Svalbard. Fan-shaped landforms were mapped using an orthophoto and digital elevation model generated from 2009 aerial photographs and a 2013 high-resolution satellite image using Geographic Information Systems. Four additional maps at a scale of 1:40,000 provide details about the morphometric characteristics of the studied fans: long- and cross-profiles, slope and aspect. Additionally, parameters such as fan and catchment area, relief, length, width, elevation (the lowest point at the fan toe, apex, and the highest point of the catchment boundary), fan mean plan and profile curvatures, fan relation to neighbouring fans, are also presented. Fans were classified according to the dominant processes shaping their surface: colluvial fans (n = 229), alluvial fans dominated by debris flows (n = 49), and alluvial fans dominated by fluvial flows (n = 19).http://dx.doi.org/10.1080/17445647.2017.1294543Colluvial fanalluvial fanremote sensingmorphometryGISPetuniabukta
collection DOAJ
language English
format Article
sources DOAJ
author Aleksandra M. Tomczyk
Marek W. Ewertowski
spellingShingle Aleksandra M. Tomczyk
Marek W. Ewertowski
Surface morphological types and spatial distribution of fan-shaped landforms in the periglacial high-Arctic environment of central Spitsbergen, Svalbard
Journal of Maps
Colluvial fan
alluvial fan
remote sensing
morphometry
GIS
Petuniabukta
author_facet Aleksandra M. Tomczyk
Marek W. Ewertowski
author_sort Aleksandra M. Tomczyk
title Surface morphological types and spatial distribution of fan-shaped landforms in the periglacial high-Arctic environment of central Spitsbergen, Svalbard
title_short Surface morphological types and spatial distribution of fan-shaped landforms in the periglacial high-Arctic environment of central Spitsbergen, Svalbard
title_full Surface morphological types and spatial distribution of fan-shaped landforms in the periglacial high-Arctic environment of central Spitsbergen, Svalbard
title_fullStr Surface morphological types and spatial distribution of fan-shaped landforms in the periglacial high-Arctic environment of central Spitsbergen, Svalbard
title_full_unstemmed Surface morphological types and spatial distribution of fan-shaped landforms in the periglacial high-Arctic environment of central Spitsbergen, Svalbard
title_sort surface morphological types and spatial distribution of fan-shaped landforms in the periglacial high-arctic environment of central spitsbergen, svalbard
publisher Taylor & Francis Group
series Journal of Maps
issn 1744-5647
publishDate 2017-11-01
description A 1:19,500 map of the Petunibukta region documents the spatial distribution of almost 300 colluvial and alluvial fans (together with their catchments) in the periglacial high-Arctic environment of Svalbard. Fan-shaped landforms were mapped using an orthophoto and digital elevation model generated from 2009 aerial photographs and a 2013 high-resolution satellite image using Geographic Information Systems. Four additional maps at a scale of 1:40,000 provide details about the morphometric characteristics of the studied fans: long- and cross-profiles, slope and aspect. Additionally, parameters such as fan and catchment area, relief, length, width, elevation (the lowest point at the fan toe, apex, and the highest point of the catchment boundary), fan mean plan and profile curvatures, fan relation to neighbouring fans, are also presented. Fans were classified according to the dominant processes shaping their surface: colluvial fans (n = 229), alluvial fans dominated by debris flows (n = 49), and alluvial fans dominated by fluvial flows (n = 19).
topic Colluvial fan
alluvial fan
remote sensing
morphometry
GIS
Petuniabukta
url http://dx.doi.org/10.1080/17445647.2017.1294543
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