From Australian Oceans Data Network
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The Cause of Breaks in Holocene Beach Ridge Progradation at Bengello Beach

Created 23/06/2025

Updated 23/06/2025

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The data that was collected for this thesis includes thermoluminescent dates, topographic surveys using a Sokkia total station, mapped stratigraphic changes sourced from the use of ground-penetrating radar (GPR), LiDAR, vegetation analyses, contemporary analogue comparison and bruun model testing, across five transects at Bengello Beach, NSW. The data was collected between 2007 and 2010. The date range of the beach ridge plain was to approximately 6000 cal BP. The data was used to identify periods of erosion and assess changes in sea level and wave climate throughout the late Holocene.

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Additional Info

Field Value
Title The Cause of Breaks in Holocene Beach Ridge Progradation at Bengello Beach
Language eng
Licence Not Specified
Landing Page https://data.gov.au/data/dataset/d41cd612-5ff3-4954-b9fc-d85e31cf852b
Contact Point
Australian Ocean Data Network
erae85@gmail.com
Reference Period 01/03/2007 - 26/05/2010
Geospatial Coverage
Map data © OpenStreetMap contributors
{
  "coordinates": [
    150.2,
    -35.8
  ],
  "type": "Point"
}
Data Portal Australian Oceans Data Network

Data Source

This dataset was originally found on Australian Oceans Data Network "The Cause of Breaks in Holocene Beach Ridge Progradation at Bengello Beach". Please visit the source to access the original metadata of the dataset:
https://catalogue.aodn.org.au/geonetwork/srv/eng/csw/dataset/the-cause-of-breaks-in-holocene-beach-ridge-progradation-at-bengello-beach