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PP66. Half Moon Bay Point (Mt Eliza) - Cliff and Platform

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 (external link) for details of geological heritage reports, and a bibliography.

Location:316729. Headland between Ranelagh Beach and Half Moon Bay, Mt Eliza.
Image: Sites of Significance Port Phillip Bay
Site 66. Apparent southerly dip of Baxter
Formation, Half Moon Bay, Mt Eliza

Access:

Canadian Bay Road, Mt Eliza.

Ownership/Managing Authority:


Crown land, Shire of Mornington

Site Description:

The site includes undercut cliffs, bluffs, a wide shore platform and backshore platform features. The most unusual feature of the site is the structure on the shore platform where ferruginous Baxter Formation sediments appear to form an anticline. Near the cliffs at Canadian Bay Road, the beds dip northeast while 100 m to the south they appear to dip to the southwest. This ‘apparent’ dip may be due to cross-bedding of sandstones. To the south of Canadian Bay Road, the cliffs decline to be scrub covered bluffs behind a wide, cobble and boulder strewn shore platform with several benched levels. These levels may be remnant platform surfaces developed at higher sea levels, but are in part structurally controlled by the cross-bedding and dip of the sandstones. There are intricate weathering patterns on the sandstone of the platform reflecting the variable composition and structure of the Baxter Formation.

Significance:

State. The site is an excellent display of the Baxter Formation and an important locality to show the lithological and structural character of that formation. It also has the most complex shore platform structure (geomorphologically and structurally) of any site in Port Phillip Bay. There are several platform levels that have been interpreted as indicating possible higher sea level sites.

Management Considerations:

Class 1. The cliffs and platform should be maintained as active coastal landforms. The most significant elements of the site are related to the shore platform, so no protective structures should be built that would obscure these. A formalised footpath leading to the southern shores of the cliffs would improve access, but this should be sited so as not to obscure the significant boulder beds on the raised platform surfaces.

References:

Gostin, V.A. (1966). Tertiary stratigraphy of the Mornington district, Victoria.
Proc. R. Soc. Vict., 79. 459-512.

Image: Sites of Significance Port Phillip Bay
Site 66. Apparent northerly dip of Baxter
Formation (Half Moon Bay, Mt Eliza)
Image: Sites of Significance Port Phillip Bay
Site 66. Benched platform levels north of
Ranelagh Beach, Mt Eliza
PP66. Half Moon Bay Point (Mt Eliza) - Cliff and PlatformSite 66. Half Moon Bay - north of Ranelagh Beach (Mt Eliza)

Image: Sites of Significance Port Phillip Bay
Site 66. Detail of apparent higher level platform
surface, North of Ranelagh Beach, Mt Eliza
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