Subglacial topography in the central Soer Rondane Mountains, East Antarctica: Configuration and morphometric analysis of valley cross profiles

In this paper an overview is given of all subglacial topography measurements carried out in the central S∅r Rondane Mountains. Data of glacier valley cross and longitudinal profiles were gathered by gravimeter and radio echo sounding measurements during former Belgian expeditions and duri...

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Main Authors: Frank Pattyn, Hugo Decleir
Format: Article
Language:English
Published: National Institute of Polar Research 1995-03-01
Series:Antarctic Record
Online Access:http://doi.org/10.15094/00008878
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spelling doaj-bfa61fb83a9a4c51a62707477d9cbd782020-11-25T01:34:26ZengNational Institute of Polar ResearchAntarctic Record0085-72892432-079X1995-03-0139112410.15094/00008878Subglacial topography in the central Soer Rondane Mountains, East Antarctica: Configuration and morphometric analysis of valley cross profilesFrank Pattyn0Hugo Decleir1 Department of Geography, Vrije Universiteit Brussel Department of Geography, Vrije Universiteit Brussel In this paper an overview is given of all subglacial topography measurements carried out in the central S∅r Rondane Mountains. Data of glacier valley cross and longitudinal profiles were gathered by gravimeter and radio echo sounding measurements during former Belgian expeditions and during the Japanese Antarctic Research Expeditions JARE-28 and JARE-32. Based on these data, a map of the subglacial topography in the central mountain area was compiled. Furthermore, a method is presented for analysing the morphometric characteristics of valley glacier cross profiles, which is shown to give beteer results than former power law equations. Finally, the morphometric analysis of the present glacierized valley cross profiles revealed a complex development regime, linked with the erosion potential of the glacierized area. http://doi.org/10.15094/00008878
collection DOAJ
language English
format Article
sources DOAJ
author Frank Pattyn
Hugo Decleir
spellingShingle Frank Pattyn
Hugo Decleir
Subglacial topography in the central Soer Rondane Mountains, East Antarctica: Configuration and morphometric analysis of valley cross profiles
Antarctic Record
author_facet Frank Pattyn
Hugo Decleir
author_sort Frank Pattyn
title Subglacial topography in the central Soer Rondane Mountains, East Antarctica: Configuration and morphometric analysis of valley cross profiles
title_short Subglacial topography in the central Soer Rondane Mountains, East Antarctica: Configuration and morphometric analysis of valley cross profiles
title_full Subglacial topography in the central Soer Rondane Mountains, East Antarctica: Configuration and morphometric analysis of valley cross profiles
title_fullStr Subglacial topography in the central Soer Rondane Mountains, East Antarctica: Configuration and morphometric analysis of valley cross profiles
title_full_unstemmed Subglacial topography in the central Soer Rondane Mountains, East Antarctica: Configuration and morphometric analysis of valley cross profiles
title_sort subglacial topography in the central soer rondane mountains, east antarctica: configuration and morphometric analysis of valley cross profiles
publisher National Institute of Polar Research
series Antarctic Record
issn 0085-7289
2432-079X
publishDate 1995-03-01
description In this paper an overview is given of all subglacial topography measurements carried out in the central S∅r Rondane Mountains. Data of glacier valley cross and longitudinal profiles were gathered by gravimeter and radio echo sounding measurements during former Belgian expeditions and during the Japanese Antarctic Research Expeditions JARE-28 and JARE-32. Based on these data, a map of the subglacial topography in the central mountain area was compiled. Furthermore, a method is presented for analysing the morphometric characteristics of valley glacier cross profiles, which is shown to give beteer results than former power law equations. Finally, the morphometric analysis of the present glacierized valley cross profiles revealed a complex development regime, linked with the erosion potential of the glacierized area.
url http://doi.org/10.15094/00008878
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AT hugodecleir subglacialtopographyinthecentralsoerrondanemountainseastantarcticaconfigurationandmorphometricanalysisofvalleycrossprofiles
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