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Mittagong Formation

Rock formation in New South Wales, Australia From Wikipedia, the free encyclopedia

Mittagong Formation
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The Mittagong Formation is a sedimentary rock unit in the Sydney Basin in eastern Australia.[1]

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Formation

Laid down in the Triassic Period, it may be seen as an interval of interbedded fine-grained sandstone and shale between the Ashfield Shale (above) and the Hawkesbury sandstone (below). The maximum thickness around Sydney may be ten metres.[2] Near Town Hall railway station, the formation is 8 metres thick. In the type area at Mittagong it is 15 metres thick.

Whereabouts

In northern Sydney it can be seen in several areas, such as West Pymble[3] and Mount Ku-ring-gai.[4] This rock formation is associated with the critically endangered Sydney Turpentine-Ironbark Forest.[5]

See also

References

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