Journey Across the Nunataks of Central East Greenland, 1951
Contains an account of a trip made in Aug. 1951 by a three-man party from the Lauge Koch expedition, which met and joined for part of the journey on the icecap, a weasel-equipped party of the French polar expedition of P.E. Victor. The main results of this trip are briefly described here; for the sc...
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Format: | Article in Journal/Newspaper |
Language: | English |
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The Arctic Institute of North America
1953
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Online Access: | https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66911 |
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ftunivcalgaryojs:oai:journalhosting.ucalgary.ca:article/66911 2023-05-15T14:19:21+02:00 Journey Across the Nunataks of Central East Greenland, 1951 Katz, H.R. 1953-01-01 application/pdf https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66911 eng eng The Arctic Institute of North America https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66911/50824 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66911 ARCTIC; Vol. 6 No. 1 (1953): March: 1–64; 2-14 1923-1245 0004-0843 Nunataks Koch Lauge 1892-1964 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion research-article 1953 ftunivcalgaryojs 2022-03-22T21:23:42Z Contains an account of a trip made in Aug. 1951 by a three-man party from the Lauge Koch expedition, which met and joined for part of the journey on the icecap, a weasel-equipped party of the French polar expedition of P.E. Victor. The main results of this trip are briefly described here; for the scientific results, maps, etc., see Arctic Bibliography No. 23166. From Ella O (72 51 N, 25 02 W) a circular route within roughly 72 30-74 N, 31-24 W was covered by plane, weasel, and the northern leg of it, devoted to the study proper, on foot. Observations on temperature, winds, ice and glacier conditions were also made during the preceding, southwestern and western leg of the journey on the weasels in cooperation with the French party. Geology of the westernmost part of central East Greenland was found to be very complex, crustal movements having apparently occurred up to the most recent epochs; it was also discovered that the Caledonian belt extends westward beyond any outcrop that can be found and, that during the Late Precambrian the geosynclinal trough had its central parts west of the present fjord-region; the western foreland of the Caledonian Syncline is therefore expected to be reached in the northernmost area, somewhere between 80 degrees and 82 degrees North. Article in Journal/Newspaper Arctic Arctic East Greenland glacier Greenland University of Calgary Journal Hosting Arctic Greenland ARCTIC 6 1 |
institution |
Open Polar |
collection |
University of Calgary Journal Hosting |
op_collection_id |
ftunivcalgaryojs |
language |
English |
topic |
Nunataks Koch Lauge 1892-1964 |
spellingShingle |
Nunataks Koch Lauge 1892-1964 Katz, H.R. Journey Across the Nunataks of Central East Greenland, 1951 |
topic_facet |
Nunataks Koch Lauge 1892-1964 |
description |
Contains an account of a trip made in Aug. 1951 by a three-man party from the Lauge Koch expedition, which met and joined for part of the journey on the icecap, a weasel-equipped party of the French polar expedition of P.E. Victor. The main results of this trip are briefly described here; for the scientific results, maps, etc., see Arctic Bibliography No. 23166. From Ella O (72 51 N, 25 02 W) a circular route within roughly 72 30-74 N, 31-24 W was covered by plane, weasel, and the northern leg of it, devoted to the study proper, on foot. Observations on temperature, winds, ice and glacier conditions were also made during the preceding, southwestern and western leg of the journey on the weasels in cooperation with the French party. Geology of the westernmost part of central East Greenland was found to be very complex, crustal movements having apparently occurred up to the most recent epochs; it was also discovered that the Caledonian belt extends westward beyond any outcrop that can be found and, that during the Late Precambrian the geosynclinal trough had its central parts west of the present fjord-region; the western foreland of the Caledonian Syncline is therefore expected to be reached in the northernmost area, somewhere between 80 degrees and 82 degrees North. |
format |
Article in Journal/Newspaper |
author |
Katz, H.R. |
author_facet |
Katz, H.R. |
author_sort |
Katz, H.R. |
title |
Journey Across the Nunataks of Central East Greenland, 1951 |
title_short |
Journey Across the Nunataks of Central East Greenland, 1951 |
title_full |
Journey Across the Nunataks of Central East Greenland, 1951 |
title_fullStr |
Journey Across the Nunataks of Central East Greenland, 1951 |
title_full_unstemmed |
Journey Across the Nunataks of Central East Greenland, 1951 |
title_sort |
journey across the nunataks of central east greenland, 1951 |
publisher |
The Arctic Institute of North America |
publishDate |
1953 |
url |
https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66911 |
geographic |
Arctic Greenland |
geographic_facet |
Arctic Greenland |
genre |
Arctic Arctic East Greenland glacier Greenland |
genre_facet |
Arctic Arctic East Greenland glacier Greenland |
op_source |
ARCTIC; Vol. 6 No. 1 (1953): March: 1–64; 2-14 1923-1245 0004-0843 |
op_relation |
https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66911/50824 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66911 |
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ARCTIC |
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6 |
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1 |
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1766291113249865728 |