New Evidence of High-Level Glacial Drainage in the White Mountains, N.H.

Abstract A newly discovered pothole field in the White Mountains, N.H., is described, and is attributed to action of melt water from the last continental glacier. Discordance of pothole orientation with slope direction is explained by inferring the presence of a retaining wall of ice which controlle...

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Published in:Journal of Glaciology
Main Author: Hattin, Donald E.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1958
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000023996
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000023996
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spelling crcambridgeupr:10.1017/s0022143000023996 2024-03-03T08:46:07+00:00 New Evidence of High-Level Glacial Drainage in the White Mountains, N.H. Hattin, Donald E. 1958 http://dx.doi.org/10.1017/s0022143000023996 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000023996 en eng Cambridge University Press (CUP) Journal of Glaciology volume 3, issue 24, page 315-319 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1958 crcambridgeupr https://doi.org/10.1017/s0022143000023996 2024-02-08T08:39:08Z Abstract A newly discovered pothole field in the White Mountains, N.H., is described, and is attributed to action of melt water from the last continental glacier. Discordance of pothole orientation with slope direction is explained by inferring the presence of a retaining wall of ice which controlled stream flow direction during the period of pothole formation. The potholes constitute the highest evidence of continental glacial drainage yet known in New England. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 3 24 315 319
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Hattin, Donald E.
New Evidence of High-Level Glacial Drainage in the White Mountains, N.H.
topic_facet Earth-Surface Processes
description Abstract A newly discovered pothole field in the White Mountains, N.H., is described, and is attributed to action of melt water from the last continental glacier. Discordance of pothole orientation with slope direction is explained by inferring the presence of a retaining wall of ice which controlled stream flow direction during the period of pothole formation. The potholes constitute the highest evidence of continental glacial drainage yet known in New England.
format Article in Journal/Newspaper
author Hattin, Donald E.
author_facet Hattin, Donald E.
author_sort Hattin, Donald E.
title New Evidence of High-Level Glacial Drainage in the White Mountains, N.H.
title_short New Evidence of High-Level Glacial Drainage in the White Mountains, N.H.
title_full New Evidence of High-Level Glacial Drainage in the White Mountains, N.H.
title_fullStr New Evidence of High-Level Glacial Drainage in the White Mountains, N.H.
title_full_unstemmed New Evidence of High-Level Glacial Drainage in the White Mountains, N.H.
title_sort new evidence of high-level glacial drainage in the white mountains, n.h.
publisher Cambridge University Press (CUP)
publishDate 1958
url http://dx.doi.org/10.1017/s0022143000023996
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000023996
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 3, issue 24, page 315-319
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000023996
container_title Journal of Glaciology
container_volume 3
container_issue 24
container_start_page 315
op_container_end_page 319
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