Long‐term rates of mass wasting in Mesters Vig, northeast Greenland: notes on a re‐survey

Re‐surveys of surviving mass‐wasting target lines established by A.L. Washburn in the late 1950s in the Mesters Vig area, northeast Greenland, are used to derive estimates of long‐term mass wasting in the area. Rates of 2.9–8.1 cm.yr−1 are calculated for a 2.5–3° slope and 1.5–30.4 cm.yr−1 for a gel...

Full description

Bibliographic Details
Published in:Permafrost and Periglacial Processes
Main Authors: Steve Carver, Naja Mikkelsen, John Woodward
Format: Article in Journal/Newspaper
Language:unknown
Subjects:
Online Access:https://doi.org/10.1002/ppp.421
id ftrepec:oai:RePEc:wly:perpro:v:13:y:2002:i:3:p:243-249
record_format openpolar
spelling ftrepec:oai:RePEc:wly:perpro:v:13:y:2002:i:3:p:243-249 2023-05-15T16:25:52+02:00 Long‐term rates of mass wasting in Mesters Vig, northeast Greenland: notes on a re‐survey Steve Carver Naja Mikkelsen John Woodward https://doi.org/10.1002/ppp.421 unknown https://doi.org/10.1002/ppp.421 article ftrepec https://doi.org/10.1002/ppp.421 2020-12-04T13:31:03Z Re‐surveys of surviving mass‐wasting target lines established by A.L. Washburn in the late 1950s in the Mesters Vig area, northeast Greenland, are used to derive estimates of long‐term mass wasting in the area. Rates of 2.9–8.1 cm.yr−1 are calculated for a 2.5–3° slope and 1.5–30.4 cm.yr−1 for a gelifluction lobe on a 15–23° slope. Compared to Washburn's short‐term measurements for the same sites these long‐term rates suggest a general increase in the rate of mass wasting in the Mesters Vig area over the last 40 years. This increase may be related to a general pattern of climatic amelioration for the east coast of Greenland. Copyright © 2002 John Wiley & Sons, Ltd. Article in Journal/Newspaper Greenland RePEc (Research Papers in Economics) Greenland Mesters Vig ENVELOPE(-23.750,-23.750,72.150,72.150) Washburn ENVELOPE(-86.133,-86.133,-77.617,-77.617) Permafrost and Periglacial Processes 13 3 243 249
institution Open Polar
collection RePEc (Research Papers in Economics)
op_collection_id ftrepec
language unknown
description Re‐surveys of surviving mass‐wasting target lines established by A.L. Washburn in the late 1950s in the Mesters Vig area, northeast Greenland, are used to derive estimates of long‐term mass wasting in the area. Rates of 2.9–8.1 cm.yr−1 are calculated for a 2.5–3° slope and 1.5–30.4 cm.yr−1 for a gelifluction lobe on a 15–23° slope. Compared to Washburn's short‐term measurements for the same sites these long‐term rates suggest a general increase in the rate of mass wasting in the Mesters Vig area over the last 40 years. This increase may be related to a general pattern of climatic amelioration for the east coast of Greenland. Copyright © 2002 John Wiley & Sons, Ltd.
format Article in Journal/Newspaper
author Steve Carver
Naja Mikkelsen
John Woodward
spellingShingle Steve Carver
Naja Mikkelsen
John Woodward
Long‐term rates of mass wasting in Mesters Vig, northeast Greenland: notes on a re‐survey
author_facet Steve Carver
Naja Mikkelsen
John Woodward
author_sort Steve Carver
title Long‐term rates of mass wasting in Mesters Vig, northeast Greenland: notes on a re‐survey
title_short Long‐term rates of mass wasting in Mesters Vig, northeast Greenland: notes on a re‐survey
title_full Long‐term rates of mass wasting in Mesters Vig, northeast Greenland: notes on a re‐survey
title_fullStr Long‐term rates of mass wasting in Mesters Vig, northeast Greenland: notes on a re‐survey
title_full_unstemmed Long‐term rates of mass wasting in Mesters Vig, northeast Greenland: notes on a re‐survey
title_sort long‐term rates of mass wasting in mesters vig, northeast greenland: notes on a re‐survey
url https://doi.org/10.1002/ppp.421
long_lat ENVELOPE(-23.750,-23.750,72.150,72.150)
ENVELOPE(-86.133,-86.133,-77.617,-77.617)
geographic Greenland
Mesters Vig
Washburn
geographic_facet Greenland
Mesters Vig
Washburn
genre Greenland
genre_facet Greenland
op_relation https://doi.org/10.1002/ppp.421
op_doi https://doi.org/10.1002/ppp.421
container_title Permafrost and Periglacial Processes
container_volume 13
container_issue 3
container_start_page 243
op_container_end_page 249
_version_ 1766014716085272576