Measured Re-advance of a Debris-covered Glacier Terminus in the President Range, Yoho National Park, British Columbia, Canada

Abstract Measurements made at the terminus of Emerald Glacier in the Rocky Mountains of Canada indicate terminal re-advance in the order of one to two metres per year sustained since 1978 at least. Re-advance is maximum along that part of the terminus which is heavily covered with supraglacial debri...

Full description

Bibliographic Details
Published in:Journal of Glaciology
Main Author: Rogerson, R.J.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1985
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000004937
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000004937
id crcambridgeupr:10.1017/s0022143000004937
record_format openpolar
spelling crcambridgeupr:10.1017/s0022143000004937 2024-03-03T08:46:07+00:00 Measured Re-advance of a Debris-covered Glacier Terminus in the President Range, Yoho National Park, British Columbia, Canada Rogerson, R.J. 1985 http://dx.doi.org/10.1017/s0022143000004937 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000004937 en eng Cambridge University Press (CUP) Journal of Glaciology volume 31, issue 107, page 13-17 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1985 crcambridgeupr https://doi.org/10.1017/s0022143000004937 2024-02-08T08:40:37Z Abstract Measurements made at the terminus of Emerald Glacier in the Rocky Mountains of Canada indicate terminal re-advance in the order of one to two metres per year sustained since 1978 at least. Re-advance is maximum along that part of the terminus which is heavily covered with supraglacial debris, where ice remains in contact with a push-moraine all summer. Re-advance may represent fluctuations of a small, responsive ice mass, or the early effects of recent climatic deterioration. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Canada British Columbia ENVELOPE(-125.003,-125.003,54.000,54.000) Journal of Glaciology 31 107 13 17
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Rogerson, R.J.
Measured Re-advance of a Debris-covered Glacier Terminus in the President Range, Yoho National Park, British Columbia, Canada
topic_facet Earth-Surface Processes
description Abstract Measurements made at the terminus of Emerald Glacier in the Rocky Mountains of Canada indicate terminal re-advance in the order of one to two metres per year sustained since 1978 at least. Re-advance is maximum along that part of the terminus which is heavily covered with supraglacial debris, where ice remains in contact with a push-moraine all summer. Re-advance may represent fluctuations of a small, responsive ice mass, or the early effects of recent climatic deterioration.
format Article in Journal/Newspaper
author Rogerson, R.J.
author_facet Rogerson, R.J.
author_sort Rogerson, R.J.
title Measured Re-advance of a Debris-covered Glacier Terminus in the President Range, Yoho National Park, British Columbia, Canada
title_short Measured Re-advance of a Debris-covered Glacier Terminus in the President Range, Yoho National Park, British Columbia, Canada
title_full Measured Re-advance of a Debris-covered Glacier Terminus in the President Range, Yoho National Park, British Columbia, Canada
title_fullStr Measured Re-advance of a Debris-covered Glacier Terminus in the President Range, Yoho National Park, British Columbia, Canada
title_full_unstemmed Measured Re-advance of a Debris-covered Glacier Terminus in the President Range, Yoho National Park, British Columbia, Canada
title_sort measured re-advance of a debris-covered glacier terminus in the president range, yoho national park, british columbia, canada
publisher Cambridge University Press (CUP)
publishDate 1985
url http://dx.doi.org/10.1017/s0022143000004937
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000004937
long_lat ENVELOPE(-125.003,-125.003,54.000,54.000)
geographic Canada
British Columbia
geographic_facet Canada
British Columbia
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 31, issue 107, page 13-17
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000004937
container_title Journal of Glaciology
container_volume 31
container_issue 107
container_start_page 13
op_container_end_page 17
_version_ 1792502023990542336