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102. Athlone - Silicified Mesozoic Sandstone

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:

Catani - 906663. Four kilometres east of Heath Hill.

Image: Sites of Significance Port Phillip Bay
Silicified Mesozoic sandstone beds in quarry at Athlone.

Access:

Lyons Road, Invermay Road.

Ownership:

Private land.

Geology:

A bedrock spur on the northern side of the Lang Lang River floodplain consists of fine grained silicified Mesozoic sandstone in beds up to three metres thick. There are also thinner bedded mudstones and coals. The induration of the sandstones may be due to the proximity of the Heath Hill Fault. The unusual hardness of this material, compared with the typical Mesozoic sediments, makes it suitable for road making and construction uses. The quarry presently being worked at the site provides extensive exposures of this rock. Abundant plant fossils - notably stem casts, moulds and leaf fragments - may be obtained. There are some small spherical sandstone balls that superficially resemble the concretions common in the Mesozoic rocks of the Otway region. These are less common in South Gippsland.

Significance:

Regional. The outcrop is an example of an unusual lithology in the Mesozoic strata.

Management:

Class 2. The general principles of quarry management apply at this site and should be consulted.

References:

Mahoney, D.J., 1921. Sandstone at Athlone.
Geol. Surv. vic. Rec.. 4.

Image: Sites of Significance Port Phillip Bay
Concretions (arrowed) in Mesozoic sandstone at Athlone.
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