Morphology, patterns and processes in the Oyster Bay headland bypass dunefield, South Africa

Studies of the dunefield systems crossing the Cape St. Francis headland in the Eastern Cape have focused on the role that wind plays in sediment transfer in coastal dunefield systems, with limited consideration of the role of water. The aim of this study was to improve understanding of the morpholog...

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Main Author: McConnachie, Lauren Bernyse
Format: Others
Language:English
Published: Rhodes University 2013
Subjects:
Online Access:http://hdl.handle.net/10962/d1001904
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spelling ndltd-netd.ac.za-oai-union.ndltd.org-rhodes-vital-48042017-07-20T04:13:33ZMorphology, patterns and processes in the Oyster Bay headland bypass dunefield, South AfricaInvestigation of the relationship between morphology, patterns and processes in a headland bypass dunefield, in the Eastern Cape, South AfricaMcConnachie, Lauren BernyseSand dune conservation -- South Africa -- Eastern CapeSand dune ecology -- South Africa -- Eastern CapeCoastal ecology -- South Africa -- Eastern CapeSedimentation and deposition -- South Africa -- Eastern CapeBeach erosion -- South Africa -- Eastern CapeCoastal zone management -- South Africa -- Eastern CapeShore protection -- South Africa -- Eastern CapeStudies of the dunefield systems crossing the Cape St. Francis headland in the Eastern Cape have focused on the role that wind plays in sediment transfer in coastal dunefield systems, with limited consideration of the role of water. The aim of this study was to improve understanding of the morphology, processes and patterns within the Oyster Bay HBD system, focussing particularly on surface water and groundwater interactions and the role of surface water in sediment transfer across the dunefield system. An extensive field survey was conducted, to collect related data, complimented by spatial and temporal analysis of the study area using GIS. The key findings from this research were the apparent differences between the western and eastern regions of the dunefield with regard to specific drivers and the respective processes and responses. Wind is the major driver of change up to and across the crest of the dunefield. In the eastern region water (ground water, surface water and the Sand River System) is the primary agent of sediment flux through processes of aggregation and slumping as well as episodic events including debris flows. This study has highlighted a need for further quantitative studies that investigate the movement of sediment through dunefield systems such as this (where water is at or near the land surface). The paradigm that sediment flux is entirely due to wind is almost certainly simplistic, and deeper understanding of these systems is neededMaiden name: Elkington, LaurenRhodes UniversityFaculty of Science, Geography2013ThesisMastersMSc177 leavespdfvital:4804http://hdl.handle.net/10962/d1001904EnglishMcConnachie, Lauren Bernyse
collection NDLTD
language English
format Others
sources NDLTD
topic Sand dune conservation -- South Africa -- Eastern Cape
Sand dune ecology -- South Africa -- Eastern Cape
Coastal ecology -- South Africa -- Eastern Cape
Sedimentation and deposition -- South Africa -- Eastern Cape
Beach erosion -- South Africa -- Eastern Cape
Coastal zone management -- South Africa -- Eastern Cape
Shore protection -- South Africa -- Eastern Cape
spellingShingle Sand dune conservation -- South Africa -- Eastern Cape
Sand dune ecology -- South Africa -- Eastern Cape
Coastal ecology -- South Africa -- Eastern Cape
Sedimentation and deposition -- South Africa -- Eastern Cape
Beach erosion -- South Africa -- Eastern Cape
Coastal zone management -- South Africa -- Eastern Cape
Shore protection -- South Africa -- Eastern Cape
McConnachie, Lauren Bernyse
Morphology, patterns and processes in the Oyster Bay headland bypass dunefield, South Africa
description Studies of the dunefield systems crossing the Cape St. Francis headland in the Eastern Cape have focused on the role that wind plays in sediment transfer in coastal dunefield systems, with limited consideration of the role of water. The aim of this study was to improve understanding of the morphology, processes and patterns within the Oyster Bay HBD system, focussing particularly on surface water and groundwater interactions and the role of surface water in sediment transfer across the dunefield system. An extensive field survey was conducted, to collect related data, complimented by spatial and temporal analysis of the study area using GIS. The key findings from this research were the apparent differences between the western and eastern regions of the dunefield with regard to specific drivers and the respective processes and responses. Wind is the major driver of change up to and across the crest of the dunefield. In the eastern region water (ground water, surface water and the Sand River System) is the primary agent of sediment flux through processes of aggregation and slumping as well as episodic events including debris flows. This study has highlighted a need for further quantitative studies that investigate the movement of sediment through dunefield systems such as this (where water is at or near the land surface). The paradigm that sediment flux is entirely due to wind is almost certainly simplistic, and deeper understanding of these systems is needed === Maiden name: Elkington, Lauren
author McConnachie, Lauren Bernyse
author_facet McConnachie, Lauren Bernyse
author_sort McConnachie, Lauren Bernyse
title Morphology, patterns and processes in the Oyster Bay headland bypass dunefield, South Africa
title_short Morphology, patterns and processes in the Oyster Bay headland bypass dunefield, South Africa
title_full Morphology, patterns and processes in the Oyster Bay headland bypass dunefield, South Africa
title_fullStr Morphology, patterns and processes in the Oyster Bay headland bypass dunefield, South Africa
title_full_unstemmed Morphology, patterns and processes in the Oyster Bay headland bypass dunefield, South Africa
title_sort morphology, patterns and processes in the oyster bay headland bypass dunefield, south africa
publisher Rhodes University
publishDate 2013
url http://hdl.handle.net/10962/d1001904
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