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7.9 Gellibrand River Meanders

This information has been developed from the publications:

  • 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 Geological and Geomorphological Significance in the Shire of Otway (1984) by Neville Rosengren.
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 (external site) section of the Geological Society of Australia website for details of geological heritage reports, and a bibliography.

Location:7-005238 to 15-970213. A five kilometre section of the Gellibrand River beginning near Mt McKenzie and extending to one kilometre below the confluence of Kennedys Creek.

Meanders of the Gellibrand River

Access:
Gellibrand River Road.

Ownership:
Crown land (River Reserve) and private land.

Geomorphology:
This site illustrates the changing meander form of the Gellibrand River along a sector of confined flood plain north of Devondale. The contorted or tortuous meander sector is on the wider flood plain near the confluence of Kennedys Creek. Unlike the river sector at Sites 7.7 and 7.10, levee banks are not well developed on the wide flood plain. The river valley is here aligned along a fault trending north-easterly to the west of the valley.

Significance:
Regional. The abrupt change in meander patterns illustrates one of the varied characteristics of the longest river in the Otway region.

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