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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Published in:ARCTIC
Main Author: Katz, H.R.
Format: Article in Journal/Newspaper
Language:English
Published: The Arctic Institute of North America 1953
Subjects:
Online Access:https://journalhosting.ucalgary.ca/index.php/arctic/article/view/66911
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spelling 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
container_title ARCTIC
container_volume 6
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