Acraman impact structure: Difference between revisions
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'''Acraman impact structure''' is a deeply eroded [[impact crater]] in the [[Gawler Ranges]] of [[South Australia]].<ref name=EIDBAcraman>{{Cite Earth Impact DB |name=Acraman |access-date=2017-10-09}}</ref> Its location is marked by Lake Acraman, a circular ephemeral [[playa lake]] about {{convert|20|km|mi}} in diameter. The discovery of the impact structure and independent discovery of its [[ejecta blanket|ejecta]] were first reported in the journal ''[[Science (journal)|Science]]'' in 1986 by [[George E. Williams (geologist)|George E. Williams]]<ref name=Williams1986>{{cite journal | author = [[George E. Williams (geologist)|George E. Williams]] | date = 1986 | title = The Acraman Impact Structure: Source of Ejecta in Late Precambrian Shales, South Australia | journal = Science | volume = 233 | issue = 4760 | pages = 200–3 | doi = 10.1126/science.233.4760.200 | pmid = 17737291 |bibcode = 1986Sci...233..200W | s2cid = 30059305 }}</ref> and [[Victor Gostin|Victor A. Gostin]].<ref name=Gostin1986>{{cite journal | author = Gostin, V.A. |author2= Haines, P.W.|author3= Jenkins, R.J.F.|author4= Compston, W.|author5= Williams, I.S. | date = 1986 | title = Impact Ejecta Horizon Within Late Precambrian Shales, Adelaide Geosyncline, South Australia | journal = Science | volume = 233 | issue = 4760 | pages = 198–200 | doi = 10.1126/science.233.4760.198 | pmid = 17737290 | bibcode=1986Sci...233..198G|s2cid= 11307364|author-link= Victor Gostin}}</ref> The evidence for impact includes the presence of [[shatter cone]]s and [[shocked quartz]] in shattered bedrock on islands within Lake Acraman. | '''Acraman impact structure''' is a deeply eroded [[impact crater]] in the [[Gawler Ranges]] of [[South Australia]].<ref name=EIDBAcraman>{{Cite Earth Impact DB |name=Acraman |access-date=2017-10-09}}</ref> Its location is marked by Lake Acraman, a circular ephemeral [[playa lake]] about {{convert|20|km|mi}} in diameter. The discovery of the impact structure and independent discovery of its [[ejecta blanket|ejecta]] were first reported in the journal ''[[Science (journal)|Science]]'' in 1986 by [[George E. Williams (geologist)|George E. Williams]]<ref name=Williams1986>{{cite journal | author = [[George E. Williams (geologist)|George E. Williams]] | date = 1986 | title = The Acraman Impact Structure: Source of Ejecta in Late Precambrian Shales, South Australia | journal = Science | volume = 233 | issue = 4760 | pages = 200–3 | doi = 10.1126/science.233.4760.200 | pmid = 17737291 |bibcode = 1986Sci...233..200W | s2cid = 30059305 }}</ref> and [[Victor Gostin|Victor A. Gostin]].<ref name=Gostin1986>{{cite journal | author = Gostin, V.A. |author2= Haines, P.W.|author3= Jenkins, R.J.F.|author4= Compston, W.|author5= Williams, I.S. | date = 1986 | title = Impact Ejecta Horizon Within Late Precambrian Shales, Adelaide Geosyncline, South Australia | journal = Science | volume = 233 | issue = 4760 | pages = 198–200 | doi = 10.1126/science.233.4760.198 | pmid = 17737290 | bibcode=1986Sci...233..198G|s2cid= 11307364|author-link= Victor Gostin}}</ref> The evidence for impact includes the presence of [[shatter cone]]s and [[shocked quartz]] in shattered bedrock on islands within Lake Acraman. | ||
The impact structure is deeply eroded, and its original size must be inferred by indirect means. Some authors estimate an original diameter of up to {{convert|85|to|90|km|mi}},<ref name=Williams2005>{{cite journal | author = Williams, G.E. |author2= Gostin, V.A. | date = 2005 | title = Acraman-Bunyeroo impact event (Ediacaran), South Australia, and environmental consequences: twenty-five years on | journal = Australian Journal of Earth Sciences | volume = 52 | issue = 4–5 | pages = 607–620 | doi = 10.1080/08120090500181036 |bibcode = 2005AuJES..52..607W |s2cid= 128751351 }}</ref> while other suggest a smaller size, perhaps only {{convert|35|to|40|km|mi}}, closer to that of the depression in which Lake Acraman is centred.<ref name=Shoemaker1996>{{cite journal | author = Shoemaker, E.M. |author2= Shoemaker, C.S. | date = 1996 | title = The Proterozoic impact record of Australia | journal = AGSO Journal of Australian Geology and Geophysics | volume = 16 | pages = 379–398 | bibcode = 1990LPICo.746...47S }}</ref> The larger size estimate would imply an energy release of 5.2 | The impact structure is deeply eroded, and its original size must be inferred by indirect means. Some authors estimate an original diameter of up to {{convert|85|to|90|km|mi}},<ref name=Williams2005>{{cite journal | author = Williams, G.E. |author2= Gostin, V.A. | date = 2005 | title = Acraman-Bunyeroo impact event (Ediacaran), South Australia, and environmental consequences: twenty-five years on | journal = Australian Journal of Earth Sciences | volume = 52 | issue = 4–5 | pages = 607–620 | doi = 10.1080/08120090500181036 |bibcode = 2005AuJES..52..607W |s2cid= 128751351 }}</ref> while other suggest a smaller size, perhaps only {{convert|35|to|40|km|mi}}, closer to that of the depression in which Lake Acraman is centred.<ref name=Shoemaker1996>{{cite journal | author = Shoemaker, E.M. |author2= Shoemaker, C.S. | date = 1996 | title = The Proterozoic impact record of Australia | journal = AGSO Journal of Australian Geology and Geophysics | volume = 16 | pages = 379–398 | bibcode = 1990LPICo.746...47S }}</ref> The larger size estimate would imply an energy release of 5.2 million [[TNT equivalent|megatons of TNT]].<ref name="Williams2005" /> | ||
The impact event is estimated to have occurred about 590 million years ago during the [[Ediacaran]]; this age is not derived from the crater itself but from the position of ejecta within nearby [[sedimentary basin]]s.<ref name="Williams2005" /> | The impact event is estimated to have occurred about 590 million years ago during the [[Ediacaran]]; this age is not derived from the crater itself but from the position of ejecta within nearby [[sedimentary basin]]s.<ref name="Williams2005" /> | ||
Latest revision as of 05:41, 12 June 2025
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Acraman impact structure is a deeply eroded impact crater in the Gawler Ranges of South Australia.[1] Its location is marked by Lake Acraman, a circular ephemeral playa lake about Template:Convert in diameter. The discovery of the impact structure and independent discovery of its ejecta were first reported in the journal Science in 1986 by George E. Williams[2] and Victor A. Gostin.[3] The evidence for impact includes the presence of shatter cones and shocked quartz in shattered bedrock on islands within Lake Acraman.
The impact structure is deeply eroded, and its original size must be inferred by indirect means. Some authors estimate an original diameter of up to Template:Convert,[4] while other suggest a smaller size, perhaps only Template:Convert, closer to that of the depression in which Lake Acraman is centred.[5] The larger size estimate would imply an energy release of 5.2 million megatons of TNT.[4]
The impact event is estimated to have occurred about 590 million years ago during the Ediacaran; this age is not derived from the crater itself but from the position of ejecta within nearby sedimentary basins.[4]
The Lake Acraman Impact Structure is listed on the South Australian Heritage Register.[6]
Ejecta layer
A widespread layer of ejecta, believed to be from the Acraman impact structure, is found within Ediacaran rocks of the Flinders Ranges at least Template:Convert east of the crater,[3] and in drill holes from the Officer Basin to the north.[7] At the time these areas were shallow sea, and the ejecta settled into mud on the sea floor. The ejecta, containing shocked minerals and small shatter cones, is composed of rock similar in age and composition to that at the crater,[3] and is associated with an iridium anomaly suggesting contamination with extraterrestrial material.[8] An evolutionary radiation within marine microorganisms (acritarchs) occurs just above the level as the ejecta layer, and some authors believe there may be a connection.[9][10] The proximity of the crater to the type area for the Ediacara Biota is noted, though probably not significant given the likely global consequences of the impact.
John Acraman
The Acraman impact structure, Lake Acraman and the nearby Acraman Creek are named after South Australian colonial businessman John Acraman.[11]
Gallery
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Landsat image of Lake Acraman; screen capture from NASA World Wind
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Oblique Landsat image of Lake Acraman draped over digital elevation model (10x vertical exaggeration), looking east towards the Flinders Ranges where ejecta has been found; screen capture from NASA World Wind.
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Orange and brown soils mix with off-white saltpans, including Lake Gairdner and Lake Everard in this true-colour image.
References
External links
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- Acraman at Earth Impact Database
- Satellite image of the region (from Google Maps)
Template:Impact cratering on Earth
- ↑ Template:Cite Earth Impact DB
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- ↑ Manning, Geoffrey H. (2012). A Glossary of South Australian Place Names - From Aaron Creek to Zion Hill. Gould Genealogy & History, 2010. Via State Library of South Australia. Retrieved 7 March 2025.