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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Language: | English |
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Cambridge University Press (CUP)
1958
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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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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 |
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3 |
container_issue |
24 |
container_start_page |
315 |
op_container_end_page |
319 |
_version_ |
1792502038530097152 |