Glacial and postglacial landscape evolution at Dogger Bank since the Last Glacial Maximum

Integrated datasets of shallow seismic reflection profiles, geotechnical logs and sediment samples for offshore windfarms can reveal landscape evolution during changes in past climate, and help understanding of responses to future changes. Dogger Bank, in the southern North Sea, is an ideal site for...

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Main Author: Emery, Andrew Richard
Format: Thesis
Language:English
Published: University of Leeds 2020
Subjects:
Online Access:https://etheses.whiterose.ac.uk/27519/
https://etheses.whiterose.ac.uk/27519/1/AREmery_thesis_corrected_clean.pdf
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spelling ftwhiterose:oai:etheses.whiterose.ac.uk:27519 2023-05-15T16:41:28+02:00 Glacial and postglacial landscape evolution at Dogger Bank since the Last Glacial Maximum Emery, Andrew Richard 2020-02-29 text https://etheses.whiterose.ac.uk/27519/ https://etheses.whiterose.ac.uk/27519/1/AREmery_thesis_corrected_clean.pdf en eng University of Leeds https://etheses.whiterose.ac.uk/27519/1/AREmery_thesis_corrected_clean.pdf Emery, Andrew Richard (2020) Glacial and postglacial landscape evolution at Dogger Bank since the Last Glacial Maximum. PhD thesis, University of Leeds. cc_by_nc_sa CC-BY-NC-SA Thesis NonPeerReviewed 2020 ftwhiterose 2023-01-30T21:27:57Z Integrated datasets of shallow seismic reflection profiles, geotechnical logs and sediment samples for offshore windfarms can reveal landscape evolution during changes in past climate, and help understanding of responses to future changes. Dogger Bank, in the southern North Sea, is an ideal site for offshore wind, and the dataset acquired for site investigation used within this thesis reveals the Late Quaternary history of the North Sea. By conducting detailed interpretation of a dense grid of seismic reflection profiles, I developed high-resolution maps of the subsurface, which were correlated to sedimentological data to interpret depositional environments and landscape evolution. A complete record of the transition from glacial, through terrestrial proglacial and paraglacial, to coastal and marine environments is preserved in the sedimentary archive. Ice-marginal dynamics of the Weichselian ice sheet are revealed in buried glacial geomorphology and 30 m-thick proglacial lake-fill sediments. Rapid ice-stream downwasting at c.27 ka was followed by a slower retreat, isolating the lake, before another rapid phase of ice retreat northward, off Dogger Bank, at c.23 ka. This rerouted meltwater supply, and proglacial rivers draining the ice margin emptied. Increased precipitation due to climate warming at c.17 ka reformed a terrestrial drainage network that incised into the glaciogenic sediments. A barrier coastline was present during marine transgression at c.9 ka. Barrier retreat and preservation was controlled by the antecedent topography, with barrier drowning on shallow slopes, and continuous overstepping on steeper slopes. The landscape evolution of Dogger Bank has revealed the role of topography, at different scales, as a long-term control on geomorphic process and location. This thesis has resulted in improved understanding of the subsurface conditions on Dogger Bank, which can improve the economics of wind turbine placement. This study emphasises the importance of subsurface datasets for both future ... Thesis Ice Sheet White Rose eTheses Online (Universities Leeds, Sheffield, York) Dogger Bank ENVELOPE(2.333,2.333,54.833,54.833)
institution Open Polar
collection White Rose eTheses Online (Universities Leeds, Sheffield, York)
op_collection_id ftwhiterose
language English
description Integrated datasets of shallow seismic reflection profiles, geotechnical logs and sediment samples for offshore windfarms can reveal landscape evolution during changes in past climate, and help understanding of responses to future changes. Dogger Bank, in the southern North Sea, is an ideal site for offshore wind, and the dataset acquired for site investigation used within this thesis reveals the Late Quaternary history of the North Sea. By conducting detailed interpretation of a dense grid of seismic reflection profiles, I developed high-resolution maps of the subsurface, which were correlated to sedimentological data to interpret depositional environments and landscape evolution. A complete record of the transition from glacial, through terrestrial proglacial and paraglacial, to coastal and marine environments is preserved in the sedimentary archive. Ice-marginal dynamics of the Weichselian ice sheet are revealed in buried glacial geomorphology and 30 m-thick proglacial lake-fill sediments. Rapid ice-stream downwasting at c.27 ka was followed by a slower retreat, isolating the lake, before another rapid phase of ice retreat northward, off Dogger Bank, at c.23 ka. This rerouted meltwater supply, and proglacial rivers draining the ice margin emptied. Increased precipitation due to climate warming at c.17 ka reformed a terrestrial drainage network that incised into the glaciogenic sediments. A barrier coastline was present during marine transgression at c.9 ka. Barrier retreat and preservation was controlled by the antecedent topography, with barrier drowning on shallow slopes, and continuous overstepping on steeper slopes. The landscape evolution of Dogger Bank has revealed the role of topography, at different scales, as a long-term control on geomorphic process and location. This thesis has resulted in improved understanding of the subsurface conditions on Dogger Bank, which can improve the economics of wind turbine placement. This study emphasises the importance of subsurface datasets for both future ...
format Thesis
author Emery, Andrew Richard
spellingShingle Emery, Andrew Richard
Glacial and postglacial landscape evolution at Dogger Bank since the Last Glacial Maximum
author_facet Emery, Andrew Richard
author_sort Emery, Andrew Richard
title Glacial and postglacial landscape evolution at Dogger Bank since the Last Glacial Maximum
title_short Glacial and postglacial landscape evolution at Dogger Bank since the Last Glacial Maximum
title_full Glacial and postglacial landscape evolution at Dogger Bank since the Last Glacial Maximum
title_fullStr Glacial and postglacial landscape evolution at Dogger Bank since the Last Glacial Maximum
title_full_unstemmed Glacial and postglacial landscape evolution at Dogger Bank since the Last Glacial Maximum
title_sort glacial and postglacial landscape evolution at dogger bank since the last glacial maximum
publisher University of Leeds
publishDate 2020
url https://etheses.whiterose.ac.uk/27519/
https://etheses.whiterose.ac.uk/27519/1/AREmery_thesis_corrected_clean.pdf
long_lat ENVELOPE(2.333,2.333,54.833,54.833)
geographic Dogger Bank
geographic_facet Dogger Bank
genre Ice Sheet
genre_facet Ice Sheet
op_relation https://etheses.whiterose.ac.uk/27519/1/AREmery_thesis_corrected_clean.pdf
Emery, Andrew Richard (2020) Glacial and postglacial landscape evolution at Dogger Bank since the Last Glacial Maximum. PhD thesis, University of Leeds.
op_rights cc_by_nc_sa
op_rightsnorm CC-BY-NC-SA
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