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4 Queenscliff Isthmus - Parallel Dune Ridges

This information has been developed from one or more of these publications:

  • Sites of Geological and Geomorphological Significance in the Westernport Bay Catchment (1984) by Neville Rosengren.
  • Sites of Geological and Geomorphological Significance in the Western Region of Melbourne (1986) by Neville Rosengren
  • Sites of Geological and Geomorphological Significance on the Coast of Port Phillip Bay (1988) by Neville Rosengren.
  • Sites of Environmental Significance in the Flood Plain of the Upper Yarra Valley Region (1983) by Neville Rosengren, Douglas Frood and Kim Lowe (as part of a study of Sites of Environmental Significance by the University of Melbourne for the then Upper Yarra Valley and Dandenong Ranges Authority).
Geological heritage sites, including sites of geomorphological interest and volcanic heritage sites, are under regular revision by the Geological Society of Australia, especially in the assessment of significance and values. Reference should be made to the most recent reports. See the Earth Science Heritage section of the Geological Society of Australia website for details of geological heritage reports, and a bibliography.

Location934612. Northern shore of Lonsdale Bay, 1.5 km west of the Point Lonsdale Lighthouse. The site includes the area south of the Bellarine Highway.
Image: Sites of Significance Port Phillip Bay
Site 4, Dune ridges forming the isthmus
at Queenscliff

Access

Coastal footpath or beach walk from Bellarine Highway and YMCA Camp.

Ownership/Managing Authority

Crown Land, Borough of Queenscliff.


Site Description

The northern shore of Lonsdale Bay is backed by parallel dune ridges forming an isthmus linking the calcarenite headlands of Point Lonsdale and Shortlands Bluff. This site represents the least modified example of this terrain. To the west of the site, the ridges are fronted by a boulder or timber seawall and groynes while to the east the topography has been modified for residential and recreational developments. The site is 300 m long extending from low water mark inland to the Bellarine Highway. There are two main scrub-covered dune ridges separated by a well pronounced swale or inter-dune corridor. Seaward to these is a grassy foredune of variable form - in places it is terraced and elsewhere is of incipient ridge form. A pattern of cut and fill is apparent along this coastal sector although it is not known on what time frame this operates. The ridges are linear to gently curving and although they must include a component of wind-blown sand to reach their height, they were apparently initiated as swash aligned ridges. No major blowouts occur across the main ridges although minor active blowouts occur on parts of the seaward dune.

Significance

Regional. These are some of the highest sand ridges on the coast of Port Phillip Bay and are a relatively intact example of high parallel ridge form. They indicate a late Holocene phase of sand nourishment to this coastal sector and of interest in sand budget studies of the Queenscliff-Swan Island area. They represent the only site on the west coast (and one of few in Port Phillip Bay) where studies of frontal dune development can be conducted.

Management Considerations

Class 2. The dunes should be maintained without protective seawalls or groynes. Techniques for dune nourishment (slat fences, sand traps), should be utilized in attempts to maintain and encourage foredune growth. Built structures that would be endangered by an episode of dune erosion should be excluded from the site. Public pathways across the dunes should be maintained to avoid excessive damage to dune vegetation that may lead to blowout development. In the event of erosion becoming excessive, beach nourishment from offshore is preferable to seawall construction at this site.

References

McArthur, J.A. (1978)

Bird, E.C.F. (1980)


Image: Sites of Significance Port Phillip Bay
Site 4, Foredune ridge, Lonsdale Bight
near Queenscliff
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