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9.1 Gellibrand River - High level prior channel

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:9-183328. Three kilometres west of Gellibrand.

Gellibrand river terraces and abandoned channel.

Access:
Carlisle-Gellibrand Road.

Ownership:
Private land.

Geomorphology:
The Gellibrand River describes a broad entrenched meander downstream from a narrow flood plain sector with three levels of terraces. The topography of the spur and the meander form suggest that a prior higher level river channel extended across the spur. Kenny (1938) reported an outcrop of brown coal in the river bank here.

Significance:
Regional. The site is of interest in determining the rates of channel incision along different sectors of the Gellibrand River. The river terraces and the high level channel are of importance in this determination.

References:
Kenny, J.P.L. (1938). "Geology of the Kawarren - Gellibrand district." Min. geol. J. Vict. 1(3): 76-79.



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