This information has been developed from one or more of these publications:
|
Location: | Catani - 906663. Four kilometres east of Heath Hill. | 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. |
Concretions (arrowed) in Mesozoic sandstone at Athlone. |