Ice-Rafted Sediments as a Cause of Some Thermokarst Lakes in the Noatak River Delta, Alaska

Irregular, barren polygonal sheets of mud scattered over the landscape of the western portion of the Noatak River Delta are derived from lake-bottom sediments, ice-rafted during flooding. The evidence suggests that the sheets of mud change the albedo and the thermal regime of the soil, induce the de...

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Published in:Science
Main Author: Ugolini, F. C.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1975
Subjects:
Online Access:http://dx.doi.org/10.1126/science.188.4183.51
https://www.science.org/doi/pdf/10.1126/science.188.4183.51
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spelling craaas:10.1126/science.188.4183.51 2024-06-09T07:49:56+00:00 Ice-Rafted Sediments as a Cause of Some Thermokarst Lakes in the Noatak River Delta, Alaska Ugolini, F. C. 1975 http://dx.doi.org/10.1126/science.188.4183.51 https://www.science.org/doi/pdf/10.1126/science.188.4183.51 en eng American Association for the Advancement of Science (AAAS) Science volume 188, issue 4183, page 51-53 ISSN 0036-8075 1095-9203 journal-article 1975 craaas https://doi.org/10.1126/science.188.4183.51 2024-05-16T12:55:23Z Irregular, barren polygonal sheets of mud scattered over the landscape of the western portion of the Noatak River Delta are derived from lake-bottom sediments, ice-rafted during flooding. The evidence suggests that the sheets of mud change the albedo and the thermal regime of the soil, induce the development of thermokarst, and lead to the formation of ponds and lakes. The angular perimeters, especially of the small ponds, support the suggested mode of formation. Article in Journal/Newspaper Thermokarst Alaska AAAS Resource Center (American Association for the Advancement of Science) Science 188 4183 51 53
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
description Irregular, barren polygonal sheets of mud scattered over the landscape of the western portion of the Noatak River Delta are derived from lake-bottom sediments, ice-rafted during flooding. The evidence suggests that the sheets of mud change the albedo and the thermal regime of the soil, induce the development of thermokarst, and lead to the formation of ponds and lakes. The angular perimeters, especially of the small ponds, support the suggested mode of formation.
format Article in Journal/Newspaper
author Ugolini, F. C.
spellingShingle Ugolini, F. C.
Ice-Rafted Sediments as a Cause of Some Thermokarst Lakes in the Noatak River Delta, Alaska
author_facet Ugolini, F. C.
author_sort Ugolini, F. C.
title Ice-Rafted Sediments as a Cause of Some Thermokarst Lakes in the Noatak River Delta, Alaska
title_short Ice-Rafted Sediments as a Cause of Some Thermokarst Lakes in the Noatak River Delta, Alaska
title_full Ice-Rafted Sediments as a Cause of Some Thermokarst Lakes in the Noatak River Delta, Alaska
title_fullStr Ice-Rafted Sediments as a Cause of Some Thermokarst Lakes in the Noatak River Delta, Alaska
title_full_unstemmed Ice-Rafted Sediments as a Cause of Some Thermokarst Lakes in the Noatak River Delta, Alaska
title_sort ice-rafted sediments as a cause of some thermokarst lakes in the noatak river delta, alaska
publisher American Association for the Advancement of Science (AAAS)
publishDate 1975
url http://dx.doi.org/10.1126/science.188.4183.51
https://www.science.org/doi/pdf/10.1126/science.188.4183.51
genre Thermokarst
Alaska
genre_facet Thermokarst
Alaska
op_source Science
volume 188, issue 4183, page 51-53
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.188.4183.51
container_title Science
container_volume 188
container_issue 4183
container_start_page 51
op_container_end_page 53
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