Polar coasts

Polar and subpolar coasts are distinctive because of extreme seasonality and the presence of ice (predominantly tidewater glaciers, ice shelves, sea ice, and ground ice). Sea ice plays a protective role but may be either erosional or constructive when mobile. Wave activity, though effective mainly d...

Full description

Bibliographic Details
Main Authors: Forbes, D.L., Hansom, J.D.
Other Authors: Flemming, B.W.
Format: Book Part
Language:unknown
Published: Elsevier 2011
Subjects:
Ice
Online Access:http://eprints.gla.ac.uk/98135/
https://doi.org/10.1016/B978-0-12-374711-2.00312-0
id ftuglasgow:oai:eprints.gla.ac.uk:98135
record_format openpolar
spelling ftuglasgow:oai:eprints.gla.ac.uk:98135 2023-05-15T13:52:36+02:00 Polar coasts Forbes, D.L. Hansom, J.D. Flemming, B.W. Hansom, J.D. 2011 http://eprints.gla.ac.uk/98135/ https://doi.org/10.1016/B978-0-12-374711-2.00312-0 unknown Elsevier Forbes, D.L. and Hansom, J.D. <http://eprints.gla.ac.uk/view/author/7128.html> (2011) Polar coasts. In: Flemming, B.W. and Hansom, J.D. (eds.) Estuarine and Coastal Geology and Geomorphology. Elsevier, pp. 245-283. ISBN 9780123747112 (doi:10.1016/B978-0-12-374711-2.00312-0 <http://dx.doi.org/10.1016/B978-0-12-374711-2.00312-0>) Book Sections NonPeerReviewed 2011 ftuglasgow https://doi.org/10.1016/B978-0-12-374711-2.00312-0 2021-09-30T22:10:31Z Polar and subpolar coasts are distinctive because of extreme seasonality and the presence of ice (predominantly tidewater glaciers, ice shelves, sea ice, and ground ice). Sea ice plays a protective role but may be either erosional or constructive when mobile. Wave activity, though effective mainly during the short summer, imposes a strong morphological signature on most sedimentary coasts. Unlithified coasts in permafrost are widespread on the Arctic Coastal Plain, where combined thermal and mechanical processes promote rapid erosion in ice-rich deposits. Antarctic and sub-Antarctic coasts are mainly dominated by rock or ice, as are parts of the Arctic coast. Book Part Antarc* Antarctic Arctic Ice Ice Shelves permafrost Sea ice University of Glasgow: Enlighten - Publications Antarctic Arctic 245 283
institution Open Polar
collection University of Glasgow: Enlighten - Publications
op_collection_id ftuglasgow
language unknown
description Polar and subpolar coasts are distinctive because of extreme seasonality and the presence of ice (predominantly tidewater glaciers, ice shelves, sea ice, and ground ice). Sea ice plays a protective role but may be either erosional or constructive when mobile. Wave activity, though effective mainly during the short summer, imposes a strong morphological signature on most sedimentary coasts. Unlithified coasts in permafrost are widespread on the Arctic Coastal Plain, where combined thermal and mechanical processes promote rapid erosion in ice-rich deposits. Antarctic and sub-Antarctic coasts are mainly dominated by rock or ice, as are parts of the Arctic coast.
author2 Flemming, B.W.
Hansom, J.D.
format Book Part
author Forbes, D.L.
Hansom, J.D.
spellingShingle Forbes, D.L.
Hansom, J.D.
Polar coasts
author_facet Forbes, D.L.
Hansom, J.D.
author_sort Forbes, D.L.
title Polar coasts
title_short Polar coasts
title_full Polar coasts
title_fullStr Polar coasts
title_full_unstemmed Polar coasts
title_sort polar coasts
publisher Elsevier
publishDate 2011
url http://eprints.gla.ac.uk/98135/
https://doi.org/10.1016/B978-0-12-374711-2.00312-0
geographic Antarctic
Arctic
geographic_facet Antarctic
Arctic
genre Antarc*
Antarctic
Arctic
Ice
Ice Shelves
permafrost
Sea ice
genre_facet Antarc*
Antarctic
Arctic
Ice
Ice Shelves
permafrost
Sea ice
op_relation Forbes, D.L. and Hansom, J.D. <http://eprints.gla.ac.uk/view/author/7128.html> (2011) Polar coasts. In: Flemming, B.W. and Hansom, J.D. (eds.) Estuarine and Coastal Geology and Geomorphology. Elsevier, pp. 245-283. ISBN 9780123747112 (doi:10.1016/B978-0-12-374711-2.00312-0 <http://dx.doi.org/10.1016/B978-0-12-374711-2.00312-0>)
op_doi https://doi.org/10.1016/B978-0-12-374711-2.00312-0
container_start_page 245
op_container_end_page 283
_version_ 1766257019598143488