Renewed Activity of Muldrow Glacier, Alaska, After the 1956 Surge
Recovery of the Muldrow Glacier in the area below the lower Muldrow ice fall is progressing at a rapid rate. About one-third of the lost ice thickness at the base of the ice fall has been replaced during the 10 years since the surge. The ice velocity in this region is apparently quite rapid, but qui...
Published in: | Journal of Glaciology |
---|---|
Main Author: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press (CUP)
1970
|
Subjects: | |
Online Access: | http://dx.doi.org/10.1017/s0022143000022930 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000022930 |
id |
crcambridgeupr:10.1017/s0022143000022930 |
---|---|
record_format |
openpolar |
spelling |
crcambridgeupr:10.1017/s0022143000022930 2024-03-03T08:44:33+00:00 Renewed Activity of Muldrow Glacier, Alaska, After the 1956 Surge Harrison, A. E. 1970 http://dx.doi.org/10.1017/s0022143000022930 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000022930 en eng Cambridge University Press (CUP) Journal of Glaciology volume 9, issue 57, page 397-400 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1970 crcambridgeupr https://doi.org/10.1017/s0022143000022930 2024-02-08T08:42:50Z Recovery of the Muldrow Glacier in the area below the lower Muldrow ice fall is progressing at a rapid rate. About one-third of the lost ice thickness at the base of the ice fall has been replaced during the 10 years since the surge. The ice velocity in this region is apparently quite rapid, but quickly decreases down-stream and is barely detectable at McGonagall Pass, 6.5 km from the base of the ice fall. Muldrow Glacier still offers an excellent opportunity to study the recovery from a surge, and the flow of a normal wave into stagnant ice. Article in Journal/Newspaper glacier Journal of Glaciology Alaska Cambridge University Press Journal of Glaciology 9 57 397 400 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Harrison, A. E. Renewed Activity of Muldrow Glacier, Alaska, After the 1956 Surge |
topic_facet |
Earth-Surface Processes |
description |
Recovery of the Muldrow Glacier in the area below the lower Muldrow ice fall is progressing at a rapid rate. About one-third of the lost ice thickness at the base of the ice fall has been replaced during the 10 years since the surge. The ice velocity in this region is apparently quite rapid, but quickly decreases down-stream and is barely detectable at McGonagall Pass, 6.5 km from the base of the ice fall. Muldrow Glacier still offers an excellent opportunity to study the recovery from a surge, and the flow of a normal wave into stagnant ice. |
format |
Article in Journal/Newspaper |
author |
Harrison, A. E. |
author_facet |
Harrison, A. E. |
author_sort |
Harrison, A. E. |
title |
Renewed Activity of Muldrow Glacier, Alaska, After the 1956 Surge |
title_short |
Renewed Activity of Muldrow Glacier, Alaska, After the 1956 Surge |
title_full |
Renewed Activity of Muldrow Glacier, Alaska, After the 1956 Surge |
title_fullStr |
Renewed Activity of Muldrow Glacier, Alaska, After the 1956 Surge |
title_full_unstemmed |
Renewed Activity of Muldrow Glacier, Alaska, After the 1956 Surge |
title_sort |
renewed activity of muldrow glacier, alaska, after the 1956 surge |
publisher |
Cambridge University Press (CUP) |
publishDate |
1970 |
url |
http://dx.doi.org/10.1017/s0022143000022930 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000022930 |
genre |
glacier Journal of Glaciology Alaska |
genre_facet |
glacier Journal of Glaciology Alaska |
op_source |
Journal of Glaciology volume 9, issue 57, page 397-400 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000022930 |
container_title |
Journal of Glaciology |
container_volume |
9 |
container_issue |
57 |
container_start_page |
397 |
op_container_end_page |
400 |
_version_ |
1792500054805708800 |