Cryogenic sediment‐filled wedges, northern Delaware, USA
Wedge‐like sedimentary structures at two sites in northern Delaware USA are located at the erosional surface of, and extend into, channel deposits of the fluvial, mid‐Pleistocene Columbia Formation. The wedges are 0.25–0.60 m wide at the top, 1.0–1.5 m in vertical extent, contain moderate to poorly...
Published in: | Permafrost and Periglacial Processes |
---|---|
Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Subjects: | |
Online Access: | https://doi.org/10.1002/ppp.481 |
id |
ftrepec:oai:RePEc:wly:perpro:v:15:y:2004:i:4:p:319-326 |
---|---|
record_format |
openpolar |
spelling |
ftrepec:oai:RePEc:wly:perpro:v:15:y:2004:i:4:p:319-326 2023-05-15T16:37:40+02:00 Cryogenic sediment‐filled wedges, northern Delaware, USA Mary D. Lemcke Frederick E. Nelson https://doi.org/10.1002/ppp.481 unknown https://doi.org/10.1002/ppp.481 article ftrepec https://doi.org/10.1002/ppp.481 2020-12-04T13:31:25Z Wedge‐like sedimentary structures at two sites in northern Delaware USA are located at the erosional surface of, and extend into, channel deposits of the fluvial, mid‐Pleistocene Columbia Formation. The wedges are 0.25–0.60 m wide at the top, 1.0–1.5 m in vertical extent, contain moderate to poorly sorted, and vertically‐stratified sediment, and are overlain unconformably by a layer of wind‐blown silt. Several hypotheses for the formation and infill of the wedges were evaluated using detailed physical, stratigraphic, and sedimentological information. The most likely explanation for the features is that they are relict cryogenic structures formed by thermal‐contraction cracking in permafrost, and filled with wind‐blown sediments derived from the Columbia Formation. The wedges are believed to have formed in the tundra environment that existed in northern Delaware, south of the Laurentide Ice Sheet, during the coldest parts of the Wisconsinan glaciation. Copyright © 2004 John Wiley & Sons, Ltd. Article in Journal/Newspaper Ice Ice Sheet permafrost Tundra wedge* RePEc (Research Papers in Economics) Permafrost and Periglacial Processes 15 4 319 326 |
institution |
Open Polar |
collection |
RePEc (Research Papers in Economics) |
op_collection_id |
ftrepec |
language |
unknown |
description |
Wedge‐like sedimentary structures at two sites in northern Delaware USA are located at the erosional surface of, and extend into, channel deposits of the fluvial, mid‐Pleistocene Columbia Formation. The wedges are 0.25–0.60 m wide at the top, 1.0–1.5 m in vertical extent, contain moderate to poorly sorted, and vertically‐stratified sediment, and are overlain unconformably by a layer of wind‐blown silt. Several hypotheses for the formation and infill of the wedges were evaluated using detailed physical, stratigraphic, and sedimentological information. The most likely explanation for the features is that they are relict cryogenic structures formed by thermal‐contraction cracking in permafrost, and filled with wind‐blown sediments derived from the Columbia Formation. The wedges are believed to have formed in the tundra environment that existed in northern Delaware, south of the Laurentide Ice Sheet, during the coldest parts of the Wisconsinan glaciation. Copyright © 2004 John Wiley & Sons, Ltd. |
format |
Article in Journal/Newspaper |
author |
Mary D. Lemcke Frederick E. Nelson |
spellingShingle |
Mary D. Lemcke Frederick E. Nelson Cryogenic sediment‐filled wedges, northern Delaware, USA |
author_facet |
Mary D. Lemcke Frederick E. Nelson |
author_sort |
Mary D. Lemcke |
title |
Cryogenic sediment‐filled wedges, northern Delaware, USA |
title_short |
Cryogenic sediment‐filled wedges, northern Delaware, USA |
title_full |
Cryogenic sediment‐filled wedges, northern Delaware, USA |
title_fullStr |
Cryogenic sediment‐filled wedges, northern Delaware, USA |
title_full_unstemmed |
Cryogenic sediment‐filled wedges, northern Delaware, USA |
title_sort |
cryogenic sediment‐filled wedges, northern delaware, usa |
url |
https://doi.org/10.1002/ppp.481 |
genre |
Ice Ice Sheet permafrost Tundra wedge* |
genre_facet |
Ice Ice Sheet permafrost Tundra wedge* |
op_relation |
https://doi.org/10.1002/ppp.481 |
op_doi |
https://doi.org/10.1002/ppp.481 |
container_title |
Permafrost and Periglacial Processes |
container_volume |
15 |
container_issue |
4 |
container_start_page |
319 |
op_container_end_page |
326 |
_version_ |
1766027962168115200 |