Past permafrost on the Mid‐Atlantic Coastal Plain, eastern United States
Sand‐wedge casts, soil wedges and other non‐diastrophic, post‐depositional sedimentary structures suggest that Late‐Pleistocene permafrost and deep seasonal frost on the Mid‐Atlantic Coastal Plain extended at least as far south as southern Delaware, the Eastern Shore and southern Maryland. Heterogen...
Published in: | Permafrost and Periglacial Processes |
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Language: | unknown |
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Online Access: | https://doi.org/10.1002/ppp.659 |
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ftrepec:oai:RePEc:wly:perpro:v:20:y:2009:i:3:p:285-294 2023-05-15T17:55:26+02:00 Past permafrost on the Mid‐Atlantic Coastal Plain, eastern United States Hugh French Mark Demitroff Wayne L. Newell https://doi.org/10.1002/ppp.659 unknown https://doi.org/10.1002/ppp.659 article ftrepec https://doi.org/10.1002/ppp.659 2020-12-04T13:31:25Z Sand‐wedge casts, soil wedges and other non‐diastrophic, post‐depositional sedimentary structures suggest that Late‐Pleistocene permafrost and deep seasonal frost on the Mid‐Atlantic Coastal Plain extended at least as far south as southern Delaware, the Eastern Shore and southern Maryland. Heterogeneous cold‐climate slope deposits mantle lower valley‐side slopes in central Maryland. A widespread pre‐existing fragipan is congruent with the inferred palaeo‐permafrost table. The high bulk density of the fragipan was probably enhanced by either thaw consolidation when icy permafrost degraded at the active layer‐permafrost interface or by liquefaction and compaction when deep seasonal frost thawed. Copyright © 2009 John Wiley & Sons, Ltd. Article in Journal/Newspaper permafrost wedge* RePEc (Research Papers in Economics) Permafrost and Periglacial Processes 20 3 285 294 |
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Open Polar |
collection |
RePEc (Research Papers in Economics) |
op_collection_id |
ftrepec |
language |
unknown |
description |
Sand‐wedge casts, soil wedges and other non‐diastrophic, post‐depositional sedimentary structures suggest that Late‐Pleistocene permafrost and deep seasonal frost on the Mid‐Atlantic Coastal Plain extended at least as far south as southern Delaware, the Eastern Shore and southern Maryland. Heterogeneous cold‐climate slope deposits mantle lower valley‐side slopes in central Maryland. A widespread pre‐existing fragipan is congruent with the inferred palaeo‐permafrost table. The high bulk density of the fragipan was probably enhanced by either thaw consolidation when icy permafrost degraded at the active layer‐permafrost interface or by liquefaction and compaction when deep seasonal frost thawed. Copyright © 2009 John Wiley & Sons, Ltd. |
format |
Article in Journal/Newspaper |
author |
Hugh French Mark Demitroff Wayne L. Newell |
spellingShingle |
Hugh French Mark Demitroff Wayne L. Newell Past permafrost on the Mid‐Atlantic Coastal Plain, eastern United States |
author_facet |
Hugh French Mark Demitroff Wayne L. Newell |
author_sort |
Hugh French |
title |
Past permafrost on the Mid‐Atlantic Coastal Plain, eastern United States |
title_short |
Past permafrost on the Mid‐Atlantic Coastal Plain, eastern United States |
title_full |
Past permafrost on the Mid‐Atlantic Coastal Plain, eastern United States |
title_fullStr |
Past permafrost on the Mid‐Atlantic Coastal Plain, eastern United States |
title_full_unstemmed |
Past permafrost on the Mid‐Atlantic Coastal Plain, eastern United States |
title_sort |
past permafrost on the mid‐atlantic coastal plain, eastern united states |
url |
https://doi.org/10.1002/ppp.659 |
genre |
permafrost wedge* |
genre_facet |
permafrost wedge* |
op_relation |
https://doi.org/10.1002/ppp.659 |
op_doi |
https://doi.org/10.1002/ppp.659 |
container_title |
Permafrost and Periglacial Processes |
container_volume |
20 |
container_issue |
3 |
container_start_page |
285 |
op_container_end_page |
294 |
_version_ |
1766163376291971072 |