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78. Tooradin - Arcuate Ridge

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:Devon Meadows – 574725. Three kilometres north-north-east of Tooradin.
Access:Muddy Gates Lane.
Ownership:Private land.
Geomorphology:A broad low ridge (less than five metres high) trends north-east across Muddy Gates Lane. The ridge has an unusual orientation in comparison with other Cranbourne Sand ridges, and has a smoothly curving western margin. It resembles in form those described at Rythedale (Site 84) and Cardinia (Site 86).
Significance:Regional. The composition and origin of this feature is not clear. It may represent a reworking of Cranbourne Sand topography at the margins of a former lake in the Dalmore Swamp.
Management:Class 2. Extensive quarrying or large scale construction activities that subsequently modified the topography of the ridge should not be permitted.
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