Minchinbury Sandstone
| Minchinbury Sandstone | |
|---|---|
| Stratigraphic range: | |
Exposed sandstone beside the Duck River, in South Granville | |
| Type | Geological formation |
| Unit of | Wiannamatta group |
| Underlies | Bringelly Shale |
| Overlies | Hawkesbury sandstone |
| Thickness | up to 6 metres (20 ft) |
| Lithology | |
| Primary | Sandstone |
| Other | Shale |
| Location | |
| Location | Sydney, Australia |
| Region | Western Sydney, south-western Sydney |
| Country | Australia |
| Type section | |
| Named for | Minchinbury |
Minchinbury Sandstone is a component of the Wianammatta Group of sedimentary rocks in the Sydney Basin of eastern Australia that was formed in the middle Triassic period.[1] The sandstone was structured by marine deposition as a set of sandy barrier islands at a coastal shoreline.[2]
Description
Thickness is between 1.5 metres (4.9 ft) and 6 metres (20 ft) , usually less than 3 metres (9.8 ft) . It comprises up to 70% quartz with calcite and volcanic lithic fragments. There is less feldspar and more calcite than the adjacent Bringelly Shale. Related to Greywacke, it comprises fine to medium-grained lithic sandstone. The sandstone is a shoreline facies containing a beach and barrier bar complex.[3]
The Bringelly Shale lies above the Minchinbury Sandstone.[4] Fossils are rare in this stratum, though plant fragments have been recorded.[5]
Location
The type locality of the formation is near the Great Western Highway in the suburb of Minchinbury in western Sydney. It is most often seen in the western parts of the city. Outcroppings are weak and not easily found, but it may be seen in places like road cuttings in localities from Epping, Grose Vale-Kurrajong, Kellyville, Rogans Hill, Bankstown, Pendle Hill, Bonnyrigg, Menangle, Duck River, Brownlow Hill and other sites.[5][6]
At Minchinbury, the sandstone is more than 100 metres (330 ft) deep in a downhole, and its natural outcrops are particularly elusive to find elsewhere. In Lansdowne, there are large, albeit disconnected sandstone slabs, with other smaller outcrops and floaters dispersed near a slope.[7]
See also
References
- ^ Chris Herbert & Robin Helby (1980). A Guide to the Sydney basin (1st ed.). Maitland, NSW: Geological Survey of NSW. p. 582. ISBN 0-7240-1250-8.
- ^ John Byrnes & Viera Scheibner. "The inorganic nature of marine microfossils described from the Wianamatta Group". Geological Survey of New South Wales. Retrieved October 24, 2012.
- ^ "Bulletin No. 25 - 1979: The Geology and Resource Potential of the Wianamatta Group". geoscience.nsw.gov. New South Wales Government. Retrieved May 31, 2025.
- ^ "Geology Of The Triassic Rocks Of The Sydney Area" (PDF). pellsconsulting.com.au. Retrieved October 24, 2012.
- ^ a b "Minchinbury Sandstone". Stratigraphic Search Geoscience Australia. Australian Government. Retrieved October 24, 2012.
- ^ Lovering, J. F., 1954. "Bringelly Shale" (PDF). STRATIGRAPHY OF' THE WIANAMATTA GROUP. Australian Museum. Retrieved August 23, 2012.
{{cite web}}: CS1 maint: multiple names: authors list (link) CS1 maint: numeric names: authors list (link) - ^ "Wianamatta Group". Step.org. Retrieved May 31, 2025.