Observation of Hollows in the Snow Surface of Torv Gletscher, East Greenland

Many elongated hollows about 300 m. long, 200 m. wide and 30 m. deep occur on the surface of Torv Gletscher in a region where the flow of the glacier splits in several directions. Their possible origin is discussed.

Bibliographic Details
Published in:Journal of Glaciology
Main Author: Rucklidge, John
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1966
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000019584
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000019584
id crcambridgeupr:10.1017/s0022143000019584
record_format openpolar
spelling crcambridgeupr:10.1017/s0022143000019584 2024-03-03T08:43:59+00:00 Observation of Hollows in the Snow Surface of Torv Gletscher, East Greenland Rucklidge, John 1966 http://dx.doi.org/10.1017/s0022143000019584 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000019584 en eng Cambridge University Press (CUP) Journal of Glaciology volume 6, issue 45, page 446-449 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1966 crcambridgeupr https://doi.org/10.1017/s0022143000019584 2024-02-08T08:40:23Z Many elongated hollows about 300 m. long, 200 m. wide and 30 m. deep occur on the surface of Torv Gletscher in a region where the flow of the glacier splits in several directions. Their possible origin is discussed. Article in Journal/Newspaper East Greenland glacier Greenland Journal of Glaciology Cambridge University Press Greenland Journal of Glaciology 6 45 446 449
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Rucklidge, John
Observation of Hollows in the Snow Surface of Torv Gletscher, East Greenland
topic_facet Earth-Surface Processes
description Many elongated hollows about 300 m. long, 200 m. wide and 30 m. deep occur on the surface of Torv Gletscher in a region where the flow of the glacier splits in several directions. Their possible origin is discussed.
format Article in Journal/Newspaper
author Rucklidge, John
author_facet Rucklidge, John
author_sort Rucklidge, John
title Observation of Hollows in the Snow Surface of Torv Gletscher, East Greenland
title_short Observation of Hollows in the Snow Surface of Torv Gletscher, East Greenland
title_full Observation of Hollows in the Snow Surface of Torv Gletscher, East Greenland
title_fullStr Observation of Hollows in the Snow Surface of Torv Gletscher, East Greenland
title_full_unstemmed Observation of Hollows in the Snow Surface of Torv Gletscher, East Greenland
title_sort observation of hollows in the snow surface of torv gletscher, east greenland
publisher Cambridge University Press (CUP)
publishDate 1966
url http://dx.doi.org/10.1017/s0022143000019584
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000019584
geographic Greenland
geographic_facet Greenland
genre East Greenland
glacier
Greenland
Journal of Glaciology
genre_facet East Greenland
glacier
Greenland
Journal of Glaciology
op_source Journal of Glaciology
volume 6, issue 45, page 446-449
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000019584
container_title Journal of Glaciology
container_volume 6
container_issue 45
container_start_page 446
op_container_end_page 449
_version_ 1792499463503216640