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17 Indented Head - Gravel Bed

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.

Location001752. Coastal cliff at Indented Head south of the jetty.
Image: Sites of Significance Port Phillip Bay
Site 17, Indented Head. Gravel and shell bed (arrowed) overlying Moorabool Viaduct sand.
AccessThe Esplanade.
Ownership/Managing AuthorityCrown land (Indented Head Foreshore Committee of Management and Department of Conservation, Forests and Lands).

Site Description

The low cliff exposes a complex section of sandstone and clayey sandstone of the Moorabool Viaduct Sand. The lower section is a firm, pale weathered sandstone overlain by a reddish-brown clayey sandstone containing large, indurated blocks. At the cliff top is a dark sand horizon 1 m thick and at the base of this is a continuous band of ferruginous gravel, containing rounded pebbles and broken shell. The sand and gravels are over 1.5 m above present high water mark, and have the appearance of a beach deposit. It is not certain whether the deposit is part of an early Pleistocene gravel and conglomerate sequence or is a Holocene higher sea level beach.

Significance

Regional. The site is an outstanding example of a classical problem in coastal sedimentary interpretation - ie - determining the origin of a ‘beach’ deposit that is apparently above the reach of wave action with the sea at its present level. The site is therefore an important teaching and research locality.

Management Considerations

Class 1. Coastal reclamation work at this cliff site should cease. Grading and filling of the cliff top, dumping of rock, rubble or cement blocks to reclaim or protect the site from erosion will, if continued, cover the exposures and thus degrade or destroy the site. Extensions to parking, boating or other facilities should be directed away from the eastern and southern sides of the headland.

References

Hills, E.S. (1940).

Jutson, J.T. (1931).


Indented Head
Site 16 & 17, Indented Head area

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