Jump to content

Dalgaranga crater: Difference between revisions

Coordinates: 27°38′6″S 117°17′20″E / 27.63500°S 117.28889°E / -27.63500; 117.28889
From Wikipedia, the free encyclopedia
Content deleted Content added
+link
AnomieBOT (talk | contribs)
m Dating maintenance tags: {{Use dmy dates}} {{Use Australian English}}
 
(13 intermediate revisions by 11 users not shown)
Line 1: Line 1:
{{Short description|Impact crater in Western Australia}}
{{use dmy dates|date=September 2023}}
{{use Australian English|date=September 2023}}
{{Infobox terrestrial impact site
{{Infobox terrestrial impact site
| name = Dalgaranga crater
| name = Dalgaranga crater
| other_name =
| other_name =
| photo = File:Meteor impact cracter - panoramio.jpg
| photo =
| photo_size =
| photo_size =
| photo_alt =
| photo_alt =
| photo_caption =
| photo_caption = The Dalgaranga crater in September 2009
| map = Western Australia
| map = Western Australia
| map_alt =
| map_alt =
Line 29: Line 32:
| topo =
| topo =
| access =
| access =
| country = {{AUS}}
| country = Australia
| state = [[Western Australia]]
| state = [[Western Australia]]
| province =
| province =
Line 35: Line 38:
| municipality =
| municipality =
}}
}}
'''Dalgaranga crater''' is a small [[meteorite]] [[impact crater]] located on Dalgaranga pastoral station 75&nbsp;km west of [[Mount Magnet, Western Australia|Mount Magnet]] (or north of [[Yalgoo, Western Australia|Yalgoo]]) in [[Western Australia]]. It is only 24 m in diameter and 3 m deep, making it Australia's smallest impact crater (with exception of the smallest members of the [[Henbury crater|Henbury crater field]]).<ref>{{cite Earth Impact DB | name = Dalgaranga| accessdate = 2009-08-19}}</ref><ref name="Bevan_1996">{{cite journal | last1 = Bevan | first1 = A.W.R. | year = 1996 | title = Australian crater-forming meteorites. AGSO | url = | journal = Journal of Australian Geology & Geophysics | volume = 16 | issue = | pages = 421–429 }}</ref> Though discovered in 1921, it was not reported in the scientific literature until 1938.<ref name="Simpson_1938">Simpson E.S. 1938. Some new and little known meteorites found in Western Australia. Mineralogical Magazine 25, 157–171.</ref> The bedrock at the site is weathered [[Archean|Archaean]] [[granite]] of the [[Yilgarn Craton]]. The discovery of fragments of [[mesosiderite]] stony-iron meteorite around the crater confirms an impact origin,<ref name="Nininger_1960">{{cite journal | last1 = Nininger | first1 = H.H. | last2 = Huss | first2 = G.I. | year = 1960 | title = The unique meteorite crater at Dalgaranga, Western Australia | url = | journal = Mineralogical Magazine | volume = 32 | issue = | pages = 619–639 | doi=10.1180/minmag.1960.032.251.03| bibcode = 1960MinM...32..619N }}</ref> making this crater unique as the only one known to have been produced by a mesosiderite projectile.<ref>{{Citation | author1=Bevan, A | author2=Griffin, Brendan | title=Re-examination of the Murchison Downs meteorite: a fragment of the Dalgaranga mesosiderite | publication-date=1994 | url=http://trove.nla.gov.au/work/205262833 | accessdate=5 November 2017 }}</ref>
'''Dalgaranga crater''' is a small [[meteorite]] [[impact crater]] located on Dalgaranga pastoral station {{cvt|75|km}} northwest of [[Mount Magnet, Western Australia|Mount Magnet]] (or north of [[Yalgoo, Western Australia|Yalgoo]]) in [[Western Australia]]. It is only {{cvt|24 |m}} in diameter and {{cvt|3 |m}} deep, making it Australia's smallest impact crater (with exception of the smallest members of the [[Henbury crater|Henbury crater field]]).<ref>{{cite Earth Impact DB | name = Dalgaranga| accessdate = 2009-08-19}}</ref><ref name="Bevan_1996">{{cite journal | last1 = Bevan | first1 = A.W.R. | year = 1996 | title = Australian crater-forming meteorites. | journal = [[AGSO Journal of Australian Geology & Geophysics]] |url=https://ecat.ga.gov.au/geonetwork/srv/eng/catalog.search#/metadata/81455 | volume = 16 | pages = 421–429 }}</ref> Though discovered in 1921, it was not reported in the scientific literature until 1938.<ref name="Simpson_1938">Simpson E.S. 1938. Some new and little known meteorites found in Western Australia. Mineralogical Magazine 25, 157–171.</ref> The bedrock at the site is weathered [[Archean|Archaean]] [[granite]] of the [[Yilgarn Craton]]. The discovery of fragments of [[mesosiderite]] stony-iron meteorite around the crater confirms an impact origin,<ref name="Nininger_1960">{{cite journal | last1 = Nininger | first1 = H.H. | last2 = Huss | first2 = G.I. | year = 1960 | title = The unique meteorite crater at Dalgaranga, Western Australia | journal = Mineralogical Magazine | volume = 32 | issue = 251| pages = 619–639 | doi=10.1180/minmag.1960.032.251.03| bibcode = 1960MinM...32..619N }}</ref> making this crater unique as the only one known to have been produced by a mesosiderite projectile.<ref>{{Citation | author1=Bevan, A | author2=Griffin, Brendan | title=Re-examination of the Murchison Downs meteorite: a fragment of the Dalgaranga mesosiderite | date=1994 | url=http://trove.nla.gov.au/work/205262833 | access-date=5 November 2017 }}</ref>


== Description ==
== Description ==
Asymmetries in the crater structure and the ejecta blanket imply that the projectile impacted at low angle from the south-southeast.<ref name="Shoemaker_etal_2005">{{cite journal | last1 = Shoemaker | first1 = E.M. | last2 = Macdonald | first2 = F. | year = | title = A. & Shoemaker C.S. 2005. Geology of five small Australian impact craters | url = http://www.tandfonline.com/doi/abs/10.1080/08120090500180921 | journal = Australian Journal of Earth Sciences | volume = 52 | issue = | pages = 529–544 | doi = 10.1080/08120090500180921 | bibcode = 2001AuJES..52..529S }}</ref> The age is not accurately constrained but must be young because it is so well preserved for its small size, and the meteorite fragments have not weathered away; some authors suggest an age of as young as 3000 years.<ref name="Shoemaker_1988">Shoemaker E.M. & Shoemaker C.S. 1988. Impact structures of Australia (1987). Lunar and Planetary Science Conference XIX, 1079–1080. [http://adsbit.harvard.edu/cgi-bin/nph-iarticle_query?bibcode=1988LPI....19.1079S Abstract]</ref>
Asymmetries in the crater structure and the ejecta blanket imply that the projectile impacted at low angle from the south-southeast.<ref name="Shoemaker_etal_2005">{{cite journal | last1 = Shoemaker | first1 = E.M. | last2 = Macdonald | first2 = F. | year = 2005| title = A. & Shoemaker C.S. 2005. Geology of five small Australian impact craters | journal = Australian Journal of Earth Sciences | volume = 52 | issue = 4–5| pages = 529–544 | doi = 10.1080/08120090500180921 | bibcode = 2001AuJES..52..529S | s2cid = 130096764 }}</ref> The age is not accurately constrained but must be young because it is so well preserved for its small size, and the meteorite fragments have not weathered away; some authors suggest an age of as young as 3000 years.<ref name="Shoemaker_1988">Shoemaker E.M. & Shoemaker C.S. 1988. Impact structures of Australia (1987). Lunar and Planetary Science Conference XIX, 1079–1080. [http://adsbit.harvard.edu/cgi-bin/nph-iarticle_query?bibcode=1988LPI....19.1079S Abstract]</ref>


== Discovery ==
== Discovery ==
The crater was discovered by an Aboriginal stockman named Billy Seward in 1921. The meteorites were found shortly after by Gerard Wellard, the station manager, when Seward took him to the site. It was not until 1923 that meteorite fragments were sent to the [[Western Australian Museum]].<ref>{{cite book|last=Wellard|first=G.E.P.|title=Bushlore: or this and that from here and there|year=1983|publisher=Artlook|location=Perth|pages=95–97}}</ref><ref>{{cite journal|last=Hamacher|first=D.W.|author2=O'Neill, C.|title=The Discovery and History of the Dalgaranga Meteorite Crater, Western Australia|journal=Australian Journal of Earth Sciences|year=2013|volume=60|issue=5|pages=637–646|arxiv=1306.0663|doi=10.1080/08120099.2013.815274|bibcode=2013AuJES..60..637H}}</ref>
The crater was discovered by an [[Aboriginal Australian|Aboriginal]] stockman named Billy Seward in 1921. The meteorites were found shortly after by Gerard Wellard, the station manager, when Seward took him to the site. It was not until 1923 that meteorite fragments were sent to the [[Western Australian Museum]].<ref>{{cite book| last=Wellard|first=G.E.P.|title=Bushlore: or this and that from here and there| year=1983| publisher=Artlook| location=Perth| pages=95–97}}</ref><ref>{{cite journal|last=Hamacher|first=D.W.|author2=O'Neill, C.|title=The Discovery and History of the Dalgaranga Meteorite Crater, Western Australia|journal=Australian Journal of Earth Sciences| year=2013| volume=60 |issue=5| pages=637–646| arxiv=1306.0663| doi=10.1080/08120099.2013.815274| bibcode=2013AuJES..60..637H| s2cid=119249953}}</ref>


== References ==
== References ==
{{portal|Geology|Western Australia|Prehistory of Oceania}}
{{portal|Geology|Western Australia}}
{{reflist|30em}}
{{reflist|30em}}


{{Impact cratering on Earth}}
{{Impact cratering on Earth}}


[[Category:Impact craters of Australia]]
[[Category:Impact craters of Western Australia]]
[[Category:Holocene impact craters]]
[[Category:Holocene impact craters]]
[[Category:Quaternary Australia]]
[[Category:Quaternary Australia]]
[[Category:Geology of Western Australia]]
[[Category:Mid West (Western Australia)]]
[[Category:Mid West (Western Australia)]]

Latest revision as of 08:59, 11 September 2023

Dalgaranga crater
The Dalgaranga crater in September 2009
Impact crater/structure
ConfidenceConfirmed
Diameter24 m (79 ft)
Depth3 m (9.8 ft)
Age?3 ka
Holocene
ExposedYes
DrilledNo
Bolide typeMesosiderite
Location
LocationYilgarn craton
Coordinates27°38′6″S 117°17′20″E / 27.63500°S 117.28889°E / -27.63500; 117.28889
CountryAustralia
StateWestern Australia
Dalgaranga crater is located in Western Australia
Dalgaranga crater
Location of the crater in Western Australia

Dalgaranga crater is a small meteorite impact crater located on Dalgaranga pastoral station 75 km (47 mi) northwest of Mount Magnet (or north of Yalgoo) in Western Australia. It is only 24 m (79 ft) in diameter and 3 m (9.8 ft) deep, making it Australia's smallest impact crater (with exception of the smallest members of the Henbury crater field).[1][2] Though discovered in 1921, it was not reported in the scientific literature until 1938.[3] The bedrock at the site is weathered Archaean granite of the Yilgarn Craton. The discovery of fragments of mesosiderite stony-iron meteorite around the crater confirms an impact origin,[4] making this crater unique as the only one known to have been produced by a mesosiderite projectile.[5]

Description

[edit]

Asymmetries in the crater structure and the ejecta blanket imply that the projectile impacted at low angle from the south-southeast.[6] The age is not accurately constrained but must be young because it is so well preserved for its small size, and the meteorite fragments have not weathered away; some authors suggest an age of as young as 3000 years.[7]

Discovery

[edit]

The crater was discovered by an Aboriginal stockman named Billy Seward in 1921. The meteorites were found shortly after by Gerard Wellard, the station manager, when Seward took him to the site. It was not until 1923 that meteorite fragments were sent to the Western Australian Museum.[8][9]

References

[edit]
  1. ^ "Dalgaranga". Earth Impact Database. Planetary and Space Science Centre University of New Brunswick Fredericton. Retrieved 19 August 2009.
  2. ^ Bevan, A.W.R. (1996). "Australian crater-forming meteorites". AGSO Journal of Australian Geology & Geophysics. 16: 421–429.
  3. ^ Simpson E.S. 1938. Some new and little known meteorites found in Western Australia. Mineralogical Magazine 25, 157–171.
  4. ^ Nininger, H.H.; Huss, G.I. (1960). "The unique meteorite crater at Dalgaranga, Western Australia". Mineralogical Magazine. 32 (251): 619–639. Bibcode:1960MinM...32..619N. doi:10.1180/minmag.1960.032.251.03.
  5. ^ Bevan, A; Griffin, Brendan (1994), Re-examination of the Murchison Downs meteorite: a fragment of the Dalgaranga mesosiderite, retrieved 5 November 2017
  6. ^ Shoemaker, E.M.; Macdonald, F. (2005). "A. & Shoemaker C.S. 2005. Geology of five small Australian impact craters". Australian Journal of Earth Sciences. 52 (4–5): 529–544. Bibcode:2001AuJES..52..529S. doi:10.1080/08120090500180921. S2CID 130096764.
  7. ^ Shoemaker E.M. & Shoemaker C.S. 1988. Impact structures of Australia (1987). Lunar and Planetary Science Conference XIX, 1079–1080. Abstract
  8. ^ Wellard, G.E.P. (1983). Bushlore: or this and that from here and there. Perth: Artlook. pp. 95–97.
  9. ^ Hamacher, D.W.; O'Neill, C. (2013). "The Discovery and History of the Dalgaranga Meteorite Crater, Western Australia". Australian Journal of Earth Sciences. 60 (5): 637–646. arXiv:1306.0663. Bibcode:2013AuJES..60..637H. doi:10.1080/08120099.2013.815274. S2CID 119249953.