Small‐scale sorted nets on glacial till, Fláajökull (Southeast Iceland) and Elisbreen (Northwest Spitsbergen)

Small sorted nets occur on glacial tills deposited since the end of 19th century by the Fláajökull (southeast Iceland) and Elisbreen (northwest Spitsbergen) glaciers. The nets have mesh diameters of 0.1 to 1.2 m. They possess a relatively flat microrelief and depth of sorting of 5 to 15 cm. Clasts w...

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Published in:Permafrost and Periglacial Processes
Main Author: Maciej Dabski
Format: Article in Journal/Newspaper
Language:unknown
Subjects:
Online Access:https://doi.org/10.1002/ppp.527
id ftrepec:oai:RePEc:wly:perpro:v:16:y:2005:i:3:p:305-310
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spelling ftrepec:oai:RePEc:wly:perpro:v:16:y:2005:i:3:p:305-310 2023-05-15T16:45:34+02:00 Small‐scale sorted nets on glacial till, Fláajökull (Southeast Iceland) and Elisbreen (Northwest Spitsbergen) Maciej Dabski https://doi.org/10.1002/ppp.527 unknown https://doi.org/10.1002/ppp.527 article ftrepec https://doi.org/10.1002/ppp.527 2020-12-04T13:31:25Z Small sorted nets occur on glacial tills deposited since the end of 19th century by the Fláajökull (southeast Iceland) and Elisbreen (northwest Spitsbergen) glaciers. The nets have mesh diameters of 0.1 to 1.2 m. They possess a relatively flat microrelief and depth of sorting of 5 to 15 cm. Clasts within the coarse domain (stony borders) and till fabric analysis display chaotic orientation. The nets within the Fláajökull moraine are more active compared with nets from the Elisbreen moraines. Despite major differences in climatic conditions between southeast Iceland and northwest Spitsbergen, it is inferred that there is no distinct difference in the sorted patterns that have developed upon the young moraines of the two glaciers. Copyright © 2005 John Wiley & Sons, Ltd. Article in Journal/Newspaper Iceland Spitsbergen RePEc (Research Papers in Economics) Fláajökull ENVELOPE(-15.651,-15.651,64.365,64.365) Permafrost and Periglacial Processes 16 3 305 310
institution Open Polar
collection RePEc (Research Papers in Economics)
op_collection_id ftrepec
language unknown
description Small sorted nets occur on glacial tills deposited since the end of 19th century by the Fláajökull (southeast Iceland) and Elisbreen (northwest Spitsbergen) glaciers. The nets have mesh diameters of 0.1 to 1.2 m. They possess a relatively flat microrelief and depth of sorting of 5 to 15 cm. Clasts within the coarse domain (stony borders) and till fabric analysis display chaotic orientation. The nets within the Fláajökull moraine are more active compared with nets from the Elisbreen moraines. Despite major differences in climatic conditions between southeast Iceland and northwest Spitsbergen, it is inferred that there is no distinct difference in the sorted patterns that have developed upon the young moraines of the two glaciers. Copyright © 2005 John Wiley & Sons, Ltd.
format Article in Journal/Newspaper
author Maciej Dabski
spellingShingle Maciej Dabski
Small‐scale sorted nets on glacial till, Fláajökull (Southeast Iceland) and Elisbreen (Northwest Spitsbergen)
author_facet Maciej Dabski
author_sort Maciej Dabski
title Small‐scale sorted nets on glacial till, Fláajökull (Southeast Iceland) and Elisbreen (Northwest Spitsbergen)
title_short Small‐scale sorted nets on glacial till, Fláajökull (Southeast Iceland) and Elisbreen (Northwest Spitsbergen)
title_full Small‐scale sorted nets on glacial till, Fláajökull (Southeast Iceland) and Elisbreen (Northwest Spitsbergen)
title_fullStr Small‐scale sorted nets on glacial till, Fláajökull (Southeast Iceland) and Elisbreen (Northwest Spitsbergen)
title_full_unstemmed Small‐scale sorted nets on glacial till, Fláajökull (Southeast Iceland) and Elisbreen (Northwest Spitsbergen)
title_sort small‐scale sorted nets on glacial till, fláajökull (southeast iceland) and elisbreen (northwest spitsbergen)
url https://doi.org/10.1002/ppp.527
long_lat ENVELOPE(-15.651,-15.651,64.365,64.365)
geographic Fláajökull
geographic_facet Fláajökull
genre Iceland
Spitsbergen
genre_facet Iceland
Spitsbergen
op_relation https://doi.org/10.1002/ppp.527
op_doi https://doi.org/10.1002/ppp.527
container_title Permafrost and Periglacial Processes
container_volume 16
container_issue 3
container_start_page 305
op_container_end_page 310
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