GLACIAL LANDFORMS AND WEATHERING PROCESSES IN THE BALCHENFJELLA REGION, EASTERN PART OF THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA

P(論文) Glacial landforms and weathering processes have been investigated in the Balchenfjella region, eastern part of the Sør Rondane Mountains, East Antarctica. This region had entirely been covered with the former ice sheet, and shows less alpine features in comparison with the other parts of the S...

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Main Authors: ハヤシ, マサヒサ, ミウラ, キヨシ, HAYASHI, Masahisa, MIURA, Kiyoshi
Language:English
Published: National Institute of Polar Research 1989
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/2591/files/KJ00002368181.pdf
https://doi.org/10.15094/00002591
https://nipr.repo.nii.ac.jp/records/2591
_version_ 1829313185531822080
author ハヤシ, マサヒサ
ミウラ, キヨシ
HAYASHI, Masahisa
MIURA, Kiyoshi
author_facet ハヤシ, マサヒサ
ミウラ, キヨシ
HAYASHI, Masahisa
MIURA, Kiyoshi
author_sort ハヤシ, マサヒサ
collection National Institute of Polar Research Repository, Japan
description P(論文) Glacial landforms and weathering processes have been investigated in the Balchenfjella region, eastern part of the Sør Rondane Mountains, East Antarctica. This region had entirely been covered with the former ice sheet, and shows less alpine features in comparison with the other parts of the Sør Rondane. Deglaciation occurred at first in the northern region, Vesthjelmen-Austharmaren area. Succeedingly, the southern part of South Balchenfjella and the mountain tops in the Bulken-Hesteskoen area became free from ice. North Balchenfjella emerged in the latest stage of deglaciation. Around the areas from Bulken to South Balchenfjella, different stage of deglaciation was probably due to the ice step which had been formed by damming of ice flow by the mountain's threshold. The step still remains behind the South Balchenfjella area. Shattering and granular disintegration are most predominant among weathering features in this region. Salt aggregations, mostly gypsum, are observed in any locality. Beautifully crystallized gypsum was predominantly found in the North Balchenfjella area. Desert varnish was also examined. Chemical analysis clearly defined that the desert varnish is a film composed of crystalline jarosite mixed with amorphous silica. The varnish coat is formed by a solution of sulfuric acid from the underlying ground. Capirally action is effective for this solution to ascend through very narrow cracks within a rock. departmental bulletin paper
genre Antarc*
Antarctica
East Antarctica
Ice Sheet
genre_facet Antarc*
Antarctica
East Antarctica
Ice Sheet
geographic East Antarctica
Sør-Rondane
Sør Rondane Mountains
Balchenfjella
Bulken
Hesteskoen
Vesthjelmen
geographic_facet East Antarctica
Sør-Rondane
Sør Rondane Mountains
Balchenfjella
Bulken
Hesteskoen
Vesthjelmen
id ftnipr:oai:nipr.repo.nii.ac.jp:00002591
institution Open Polar
language English
long_lat ENVELOPE(25.000,25.000,-72.000,-72.000)
ENVELOPE(25.000,25.000,-72.000,-72.000)
ENVELOPE(27.200,27.200,-72.000,-72.000)
ENVELOPE(27.233,27.233,-71.867,-71.867)
ENVELOPE(27.583,27.583,-71.875,-71.875)
ENVELOPE(26.417,26.417,-71.683,-71.683)
op_collection_id ftnipr
op_doi https://doi.org/10.15094/00002591
op_relation Proceedings of the NIPR Symposium on Antarctic Geosciences
3
65
80
AA1072335X
https://nipr.repo.nii.ac.jp/record/2591/files/KJ00002368181.pdf
https://doi.org/10.15094/00002591
https://nipr.repo.nii.ac.jp/records/2591
publishDate 1989
publisher National Institute of Polar Research
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00002591 2025-04-13T14:08:30+00:00 GLACIAL LANDFORMS AND WEATHERING PROCESSES IN THE BALCHENFJELLA REGION, EASTERN PART OF THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA ハヤシ, マサヒサ ミウラ, キヨシ HAYASHI, Masahisa MIURA, Kiyoshi 1989-09 application/pdf https://nipr.repo.nii.ac.jp/record/2591/files/KJ00002368181.pdf https://doi.org/10.15094/00002591 https://nipr.repo.nii.ac.jp/records/2591 eng eng National Institute of Polar Research Proceedings of the NIPR Symposium on Antarctic Geosciences 3 65 80 AA1072335X https://nipr.repo.nii.ac.jp/record/2591/files/KJ00002368181.pdf https://doi.org/10.15094/00002591 https://nipr.repo.nii.ac.jp/records/2591 1989 ftnipr https://doi.org/10.15094/00002591 2025-03-19T10:19:57Z P(論文) Glacial landforms and weathering processes have been investigated in the Balchenfjella region, eastern part of the Sør Rondane Mountains, East Antarctica. This region had entirely been covered with the former ice sheet, and shows less alpine features in comparison with the other parts of the Sør Rondane. Deglaciation occurred at first in the northern region, Vesthjelmen-Austharmaren area. Succeedingly, the southern part of South Balchenfjella and the mountain tops in the Bulken-Hesteskoen area became free from ice. North Balchenfjella emerged in the latest stage of deglaciation. Around the areas from Bulken to South Balchenfjella, different stage of deglaciation was probably due to the ice step which had been formed by damming of ice flow by the mountain's threshold. The step still remains behind the South Balchenfjella area. Shattering and granular disintegration are most predominant among weathering features in this region. Salt aggregations, mostly gypsum, are observed in any locality. Beautifully crystallized gypsum was predominantly found in the North Balchenfjella area. Desert varnish was also examined. Chemical analysis clearly defined that the desert varnish is a film composed of crystalline jarosite mixed with amorphous silica. The varnish coat is formed by a solution of sulfuric acid from the underlying ground. Capirally action is effective for this solution to ascend through very narrow cracks within a rock. departmental bulletin paper Other/Unknown Material Antarc* Antarctica East Antarctica Ice Sheet National Institute of Polar Research Repository, Japan East Antarctica Sør-Rondane ENVELOPE(25.000,25.000,-72.000,-72.000) Sør Rondane Mountains ENVELOPE(25.000,25.000,-72.000,-72.000) Balchenfjella ENVELOPE(27.200,27.200,-72.000,-72.000) Bulken ENVELOPE(27.233,27.233,-71.867,-71.867) Hesteskoen ENVELOPE(27.583,27.583,-71.875,-71.875) Vesthjelmen ENVELOPE(26.417,26.417,-71.683,-71.683)
spellingShingle ハヤシ, マサヒサ
ミウラ, キヨシ
HAYASHI, Masahisa
MIURA, Kiyoshi
GLACIAL LANDFORMS AND WEATHERING PROCESSES IN THE BALCHENFJELLA REGION, EASTERN PART OF THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA
title GLACIAL LANDFORMS AND WEATHERING PROCESSES IN THE BALCHENFJELLA REGION, EASTERN PART OF THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA
title_full GLACIAL LANDFORMS AND WEATHERING PROCESSES IN THE BALCHENFJELLA REGION, EASTERN PART OF THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA
title_fullStr GLACIAL LANDFORMS AND WEATHERING PROCESSES IN THE BALCHENFJELLA REGION, EASTERN PART OF THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA
title_full_unstemmed GLACIAL LANDFORMS AND WEATHERING PROCESSES IN THE BALCHENFJELLA REGION, EASTERN PART OF THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA
title_short GLACIAL LANDFORMS AND WEATHERING PROCESSES IN THE BALCHENFJELLA REGION, EASTERN PART OF THE SØR RONDANE MOUNTAINS, EAST ANTARCTICA
title_sort glacial landforms and weathering processes in the balchenfjella region, eastern part of the sør rondane mountains, east antarctica
url https://nipr.repo.nii.ac.jp/record/2591/files/KJ00002368181.pdf
https://doi.org/10.15094/00002591
https://nipr.repo.nii.ac.jp/records/2591