Connolly Basin is a 9 km-diameter

impact crater An impact crater is a depression (geology), depression in the surface of a solid astronomical body formed by the hypervelocity impact event, impact of a smaller object. In contrast to volcanic craters, which result from explosion or internal c ...

located in the Gibson Desert of central

Western Australia Western Australia (WA) is the westernmost state of Australia. It is bounded by the Indian Ocean to the north and west, the Southern Ocean to the south, the Northern Territory to the north-east, and South Australia to the south-east. Western Aust ...

. It lies adjacent to the Talawana Track 45 km west of the junction (Windy Corner) with the Gary Highway, but is difficult to access due to the remoteness of the area. It was originally thought to be a diapir (

salt dome A salt dome is a type of structural dome formed when salt (or other evaporite minerals) intrudes into overlying rocks in a process known as diapirism. Salt domes can have unique surface and subsurface structures, and they can be discovered us ...

); an impact origin was first proposed in 1985.Shoemaker E.M. & Shoemaker C.S. 1985. Impact structures of Western Australia. 48th Annual Meeting of the Meteoritical Society, Abstracts. Meteoritics 20, 754-75

/ref>^,Shoemaker E.M. & Shoemaker C.S. 1986. Connolly Basin: a probable eroded impact crater in Western Australia. Lunar and Planetary Science Conference XVII, Abstracts, p. 797-79

/ref>

Description

Connolly Basin Western Australia oblique

The depression has a topographic rim 25–30 m high, while the centre displays a slight circular rise about 1 km in diameter and 5 m high exposing strongly deformed and steeply dipping bedrock interpreted as a central uplift.Shoemaker E.M. & Shoemaker C.S. 1989. Geology of the Connolly Basin impact structure, Western Australia. In: Lunar and Planetary Science Conference XX, Abstracts p. 1008-100

/ref>^,Shoemaker E.M., Plescia J.B., Shoemaker C.S. 2001. Connolly Basin Impact Structure, Western Australia. Lunar and Planetary Science Conference XXXII, Abstract no. 131
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Sedimentary rock Sedimentary rocks are types of rock (geology), rock formed by the cementation (geology), cementation of sediments—i.e. particles made of minerals (geological detritus) or organic matter (biological detritus)—that have been accumulated or de ...

s comprising the rim are of Early

Cretaceous The Cretaceous ( ) is a geological period that lasted from about 143.1 to 66 mya (unit), million years ago (Mya). It is the third and final period of the Mesozoic Era (geology), Era, as well as the longest. At around 77.1 million years, it is the ...

to Palaeogene age, while uplifted rocks in the centre are likely of Early Permian age, all part of the Canning Basin; the impact event itself is inferred to be of

Paleocene The Paleocene ( ), or Palaeocene, is a geological epoch (geology), epoch that lasted from about 66 to 56 mya (unit), million years ago (mya). It is the first epoch of the Paleogene Period (geology), Period in the modern Cenozoic Era (geology), ...

(early

Paleogene The Paleogene Period ( ; also spelled Palaeogene or Palæogene) is a geologic period and system that spans 43 million years from the end of the Cretaceous Period Ma (million years ago) to the beginning of the Neogene Period Ma. It is the fir ...

) age or later.^,

References

{{Impact cratering on Earth Impact craters of Western Australia Paleocene impact craters Paleocene Australia