Noen isavsmeltningsfenomener i Østerdalen.
Some features from the melting of the inland ice in Østerdalen: A few of the more large-scale features formed by melting water of the last ice sheet are described. The last part of the inland ice filled the valleys in the East Central Norway. In the valley of Østerdalen the highest point was, at a l...
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Language: | Norwegian |
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1954
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ftnorgesgu:oai:openarchive.ngu.no:11250/2674622 2023-05-15T16:40:49+02:00 Noen isavsmeltningsfenomener i Østerdalen. Oftedahl, Chr. 19171 Evenstad 19184 Hanestad 19183 Stor-Elvdal 19182 Storsjøen RENDALEN STOR-ELVDAL 1954 application/pdf https://hdl.handle.net/11250/2674622 nor nor NGU (188) https://hdl.handle.net/11250/2674622 Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no CC-BY 21-28 GLASIALGEOLOGI AVSETNING ISAVSMELTING BRESJØAVSETNING STRANDAVSETNING STRANDFLATE Journal article 1954 ftnorgesgu 2022-07-03T15:26:15Z Some features from the melting of the inland ice in Østerdalen: A few of the more large-scale features formed by melting water of the last ice sheet are described. The last part of the inland ice filled the valleys in the East Central Norway. In the valley of Østerdalen the highest point was, at a late stage, situated within the area of fig. 1. Ice-dammed lakes were formed, and various stages of the last lakes, visible as shore-lines at Atna are discussed. A lateral drainage channel, falling to the north and the Snippdalen channel, falling to the south, suggest \"4\" of fig. 1 as the most likely position for the water divide caused by the ice body in the valley. When this divide was lowered to 508 m, it was broken through. 35553 Article in Journal/Newspaper Ice Sheet NGU Open Archive (Geological Survey of Norway) Norway Østerdalen ENVELOPE(13.554,13.554,66.432,66.432) |
institution |
Open Polar |
collection |
NGU Open Archive (Geological Survey of Norway) |
op_collection_id |
ftnorgesgu |
language |
Norwegian |
topic |
GLASIALGEOLOGI AVSETNING ISAVSMELTING BRESJØAVSETNING STRANDAVSETNING STRANDFLATE |
spellingShingle |
GLASIALGEOLOGI AVSETNING ISAVSMELTING BRESJØAVSETNING STRANDAVSETNING STRANDFLATE Oftedahl, Chr. Noen isavsmeltningsfenomener i Østerdalen. |
topic_facet |
GLASIALGEOLOGI AVSETNING ISAVSMELTING BRESJØAVSETNING STRANDAVSETNING STRANDFLATE |
description |
Some features from the melting of the inland ice in Østerdalen: A few of the more large-scale features formed by melting water of the last ice sheet are described. The last part of the inland ice filled the valleys in the East Central Norway. In the valley of Østerdalen the highest point was, at a late stage, situated within the area of fig. 1. Ice-dammed lakes were formed, and various stages of the last lakes, visible as shore-lines at Atna are discussed. A lateral drainage channel, falling to the north and the Snippdalen channel, falling to the south, suggest \"4\" of fig. 1 as the most likely position for the water divide caused by the ice body in the valley. When this divide was lowered to 508 m, it was broken through. 35553 |
format |
Article in Journal/Newspaper |
author |
Oftedahl, Chr. |
author_facet |
Oftedahl, Chr. |
author_sort |
Oftedahl, Chr. |
title |
Noen isavsmeltningsfenomener i Østerdalen. |
title_short |
Noen isavsmeltningsfenomener i Østerdalen. |
title_full |
Noen isavsmeltningsfenomener i Østerdalen. |
title_fullStr |
Noen isavsmeltningsfenomener i Østerdalen. |
title_full_unstemmed |
Noen isavsmeltningsfenomener i Østerdalen. |
title_sort |
noen isavsmeltningsfenomener i østerdalen. |
publishDate |
1954 |
url |
https://hdl.handle.net/11250/2674622 |
op_coverage |
19171 Evenstad 19184 Hanestad 19183 Stor-Elvdal 19182 Storsjøen RENDALEN STOR-ELVDAL |
long_lat |
ENVELOPE(13.554,13.554,66.432,66.432) |
geographic |
Norway Østerdalen |
geographic_facet |
Norway Østerdalen |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
21-28 |
op_relation |
NGU (188) https://hdl.handle.net/11250/2674622 |
op_rights |
Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no |
op_rightsnorm |
CC-BY |
_version_ |
1766031243230576640 |