The distribution and magnitude of subglacial erosion on millennial timescales at Engabreen, Norway
We quantify the magnitude of millennial-scale glacial erosion at Engabreen, a temperate glacier in coastal northern Norway, using the in situ cosmogenic nuclides carbon-14 (14C) and beryllium-10 (10Be) in bedrock exposed recently by glacial retreat. Nuclide concentrations show no dependence on dista...
Published in: | Annals of Glaciology |
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Language: | English |
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Cambridge University Press
2019
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ftdoajarticles:oai:doaj.org/article:00f5702a63ed4717befe8bb6f272d90f 2023-05-15T13:29:34+02:00 The distribution and magnitude of subglacial erosion on millennial timescales at Engabreen, Norway Cari Rand Brent M. Goehring 2019-12-01T00:00:00Z https://doi.org/10.1017/aog.2019.42 https://doaj.org/article/00f5702a63ed4717befe8bb6f272d90f EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0260305519000429/type/journal_article https://doaj.org/toc/0260-3055 https://doaj.org/toc/1727-5644 doi:10.1017/aog.2019.42 0260-3055 1727-5644 https://doaj.org/article/00f5702a63ed4717befe8bb6f272d90f Annals of Glaciology, Vol 60, Pp 73-81 (2019) Beryllium-10 carbon-14 cosmogenic nuclides Engabreen glacial erosion Meteorology. Climatology QC851-999 article 2019 ftdoajarticles https://doi.org/10.1017/aog.2019.42 2023-03-12T01:31:55Z We quantify the magnitude of millennial-scale glacial erosion at Engabreen, a temperate glacier in coastal northern Norway, using the in situ cosmogenic nuclides carbon-14 (14C) and beryllium-10 (10Be) in bedrock exposed recently by glacial retreat. Nuclide concentrations show no dependence on distance down or across the valley. As such, resulting Holocene erosion depths along two transects perpendicular to glacier flow are highly variable with no systematic distribution, ranging from 0.10 to 2.95 m. We observed 14C–10Be ratios elevated above the production ratio in samples of abraded bedrock, which is counter to the expectation for surfaces covered during the Holocene and exposed only recently. Muon reactions produce nuclides at greater depths than do spallation reactions and 14C at production rates at higher than those of 10Be, resulting in 14C–10Be ratios that increase with depth. Therefore, elevated 14C–10Be ratios indicate that sampled sites were deeply plucked during recent cover, the Little Ice Age in this case, and then rapidly abraded prior to retreat. Our results suggest that, while glacial erosion can generate a u-shaped valley profile over long periods of time (e.g., 105–107 years), the discontinuous nature of glacial plucking produces spatially variable patterns of erosion over shorter millennial timescales. Article in Journal/Newspaper Annals of Glaciology glacier Northern Norway Directory of Open Access Journals: DOAJ Articles Engabreen ENVELOPE(13.771,13.771,66.682,66.682) Norway Annals of Glaciology 60 80 73 81 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Beryllium-10 carbon-14 cosmogenic nuclides Engabreen glacial erosion Meteorology. Climatology QC851-999 |
spellingShingle |
Beryllium-10 carbon-14 cosmogenic nuclides Engabreen glacial erosion Meteorology. Climatology QC851-999 Cari Rand Brent M. Goehring The distribution and magnitude of subglacial erosion on millennial timescales at Engabreen, Norway |
topic_facet |
Beryllium-10 carbon-14 cosmogenic nuclides Engabreen glacial erosion Meteorology. Climatology QC851-999 |
description |
We quantify the magnitude of millennial-scale glacial erosion at Engabreen, a temperate glacier in coastal northern Norway, using the in situ cosmogenic nuclides carbon-14 (14C) and beryllium-10 (10Be) in bedrock exposed recently by glacial retreat. Nuclide concentrations show no dependence on distance down or across the valley. As such, resulting Holocene erosion depths along two transects perpendicular to glacier flow are highly variable with no systematic distribution, ranging from 0.10 to 2.95 m. We observed 14C–10Be ratios elevated above the production ratio in samples of abraded bedrock, which is counter to the expectation for surfaces covered during the Holocene and exposed only recently. Muon reactions produce nuclides at greater depths than do spallation reactions and 14C at production rates at higher than those of 10Be, resulting in 14C–10Be ratios that increase with depth. Therefore, elevated 14C–10Be ratios indicate that sampled sites were deeply plucked during recent cover, the Little Ice Age in this case, and then rapidly abraded prior to retreat. Our results suggest that, while glacial erosion can generate a u-shaped valley profile over long periods of time (e.g., 105–107 years), the discontinuous nature of glacial plucking produces spatially variable patterns of erosion over shorter millennial timescales. |
format |
Article in Journal/Newspaper |
author |
Cari Rand Brent M. Goehring |
author_facet |
Cari Rand Brent M. Goehring |
author_sort |
Cari Rand |
title |
The distribution and magnitude of subglacial erosion on millennial timescales at Engabreen, Norway |
title_short |
The distribution and magnitude of subglacial erosion on millennial timescales at Engabreen, Norway |
title_full |
The distribution and magnitude of subglacial erosion on millennial timescales at Engabreen, Norway |
title_fullStr |
The distribution and magnitude of subglacial erosion on millennial timescales at Engabreen, Norway |
title_full_unstemmed |
The distribution and magnitude of subglacial erosion on millennial timescales at Engabreen, Norway |
title_sort |
distribution and magnitude of subglacial erosion on millennial timescales at engabreen, norway |
publisher |
Cambridge University Press |
publishDate |
2019 |
url |
https://doi.org/10.1017/aog.2019.42 https://doaj.org/article/00f5702a63ed4717befe8bb6f272d90f |
long_lat |
ENVELOPE(13.771,13.771,66.682,66.682) |
geographic |
Engabreen Norway |
geographic_facet |
Engabreen Norway |
genre |
Annals of Glaciology glacier Northern Norway |
genre_facet |
Annals of Glaciology glacier Northern Norway |
op_source |
Annals of Glaciology, Vol 60, Pp 73-81 (2019) |
op_relation |
https://www.cambridge.org/core/product/identifier/S0260305519000429/type/journal_article https://doaj.org/toc/0260-3055 https://doaj.org/toc/1727-5644 doi:10.1017/aog.2019.42 0260-3055 1727-5644 https://doaj.org/article/00f5702a63ed4717befe8bb6f272d90f |
op_doi |
https://doi.org/10.1017/aog.2019.42 |
container_title |
Annals of Glaciology |
container_volume |
60 |
container_issue |
80 |
container_start_page |
73 |
op_container_end_page |
81 |
_version_ |
1766001312328056832 |