List of unconfirmed impact craters on Earth
This list of unconfirmed impact craters on Earth includes only unconfirmed and theoretical impact sites that have appeared several times in the literature, or endorsed by the Impact Field Studies Group, but have not yet been confirmed by the Earth Impact Database.
Unconfirmed impact craters
The following are officially considered "unconfirmed". Due to stringent requirements regarding evidence and peer-reviewed publication, newly discovered craters, or those where collecting evidence is difficult, generally are known for some time before becoming listed.
Younger than one million years old
The first table contains unconfirmed craters younger than one million years old and at least 100 meters in diameter. The Cheko crater is thought to be the result of the famous Tunguska event. There is a highly speculative conjecture about the Sirente impact (c. 320 ± 90 AD) and its effect on the Roman empire.[1] The Burckle crater and Umm al Binni structure are proposed to be behind the floods that affected Sumerian civilization.[2][3] The age of the Bloody Creek crater is disputed, with some evidence suggesting it hit glacier ice 12000 years ago, coeval with the Younger Dryas.[4]
As the trend in the Earth Impact Database for about 25 confirmed craters younger than 800,000 years show that none is more than 2 km in diameter (except the 4 km Rio Cuarto), the chances that two large craters, Mahuika (20 km) and Burckle (30 km), forming within the last few millennia has been met with skepticism.[12][13][14]
However, the source of the enormous Australasian strewnfield (c. 800 ka) is suggested to be a crater about 100 km across somewhere in Indochina,[10][15] with Hartung and Koeberl (1994) proposing the elongated 100 km x 35 km Tonlé Sap lake in Cambodia (visible in the map at the side)[16] as a suspect structure.
Older than one million years old
The 41 craters in the table below are either older than 1 Ma, or have an unknown age.
The Decorah crater has been proposed as being part of the Ordovician meteor event.[33] The age of Silverpit and the confirmed Boltysh crater (65.17 ± 0.64 Ma), as well as their latitude, has led to the speculative hypothesis that there may have been several impacts during the KT boundary.[34][35]
The Rubielos de la Cérida and Auzara impact structures of 30-40 Ma have been considered to be companion events.[36]
The Eltanin impact has been confirmed (via an iridium anomaly and meteoritic material from ocean cores) but, as it fell into the Pacific Ocean, no crater was formed.
Craters larger than 100 km in the Phanerozoic (after 541 Ma) are notable for their size as well as for the possible coeval events associated with them especially the major extinction events.
For example, the Ishim impact structure[26] is conjectured to be bounded by the late Ordivician-early Silurian,[27] the East Warburton Basin has been linked to the Late Devonian extinction,[23] both Bedout and the Wilkes Land crater have been connected to the severe Permian–Triassic extinction event,[37][38] while the consensus is the Chicxulub impact caused the Cretaceous–Paleogene extinction event.
However, other extinction theories employ coeval periods of massive volcanism such as the Siberian Traps.
Mistaken identity
Some geological processes can result in circular or near-circular features that may be mistaken for impact craters. Some examples are calderas, sinkholes, glacial cirques, ring dikes, salt domes, and others. Conversely, an impact crater may originally be thought as one of these geological features, like Meteor crater (as a caldera) or Upheaval Dome (as a salt dome). The presence of shock metamorphism and shatter cones are important criteria in favor of an impact interpretation.
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Crater Lake, Oregon (a caldera)
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Great Blue Hole, Belize (a sinkhole)
See also
- Impact craters
- Impact events
- List of impact craters on Earth
- List of meteor air bursts
- Earth Impact Database
- Impact Field Studies Group
- Tollmann's hypothetical bolide
- Traces of Catastrophe book from Lunar and Planetary Institute - comprehensive reference on impact crater science
References
- ↑ Whitehouse, David (2003-06-23). "Space impact 'saved Christianity'". BBC News. British Broadcasting Corporation. Retrieved 2009-09-10.
- ↑ Sandra Blakeslee. "Ancient Crash, Epic Wave".
- ↑ Master, S. (2002) Umm al Binni lake, a possible Holocene impact structure in the marshes of southern Iraq: Geological evidence for its age, and implications for Bronze-age Mesopotamia. In: Leroy, S. and Stewart, I.S. (Eds.), Environmental Catastrophes and Recovery in the Holocene, Abstracts Volume, Department of Geography, Brunel University, Uxbridge, West London, UK, 29 August - 2 September 2002, pp. 56–57
- 1 2 Stevens, G, I Spooner, J Morrow, P Pufahl, R Raeside, RAF Grieve, CR Stanley, SM Barr, and D McMullin (2008) Physical evidence of a late-glacial (Younger Dryas?) impact event in southwestern Nova Scotia. Atlantic Geology. 44:42.
- 1 2 "The enigmatic Zerelia twin-lakes (Thessaly, Central Greece): two potential meteorite impact Craters". Solid Earth Discussions 5: 1511–1573. 2013. Bibcode:2013SolED...5.1511D. doi:10.5194/sed-5-1511-2013.
- ↑ Heinrich, P.V. (2003) Possible Meteorite Impact Crater in St. Helena Parish, Louisiana. Search and Discovery Article. no. 50006. American Association of Petroleum Geologist, Tulsa, Oklahoma. Retrieved March 27, 2011.
- ↑ Cannon, P.J. (1977) Meteorite impact crater discovered in central alaska with landsat imagery, Science, 1977 Jun 17;196(4296):1322-4.
- ↑ Ned Rozell (2008) The mystery of mammoth tusks with iron fillings
- ↑ Harris, R. S.; Schultz, P. H.; Zárate, M. A. (2007) La Dulce Crater: Evidence For A 2.8 Km Impact Structure In The Eastern Pampas Of Argentina, 38th Lunar and Planetary Science Conference
- 1 2 Povenmire H., Liu W. and Xianlin I. (1999) "Australasian tektites found in Guangxi Province, China", 30th Annual Lunar and Planetary Science Conference, Houston, March 1999.
- ↑ H. Povenmire, R.S. Harris, and J.H. Cornec (2011), The New Central American Tektite Strewn Field, 42nd Lunar and Planetary Science Conference (2011)
- ↑ Goff, James; et al. (2010). "Analysis of the Mahuika comet impact tsunami hypothesis". Marine Geology 271 (3/4): 292–296. doi:10.1016/j.margeo.2010.02.020.
- ↑ Bourgeois, J., and R. Weiss (2009) 'Chevrons' are not mega-tsunami deposits; a sedimentologic assessment. Geology. 37(5):403-406.
- ↑ Pinter, N., and S.E. Ishman, S.E. (2008). Impacts, mega-tsunami, and other extraordinary claims. GSA Today. 18(1):37.
- ↑ Glass B.P. and Pizzuto J.E. (1994) "Geographic variation in Australasian microtektite concentrations: Implications concerning the location and size of the source crater," J of Geophysical Research, vol 99, no E9, 19075-19081, Sept 1994.
- ↑ Hartung J. and Koberl C. (1994) "In search of the Australasian tektite source crater: the Tonle sap hypothesis", Meteoritics.
- 1 2 "Space impact clue in Antarctica".
- 1 2 L. P. Hrjanina (Khryanina). "Once again about Kainozoic meteorite structures in the Ross Sea, Antarctica" (PDF).
- ↑ Gerard-Little, P., Abbott, D., Breger, D. and Burckle, L (2006). "Evidence for a Possible Late Pliocene Impact in the Ross Sea, Antarctica".
- ↑ UQ Researcher Discovers Giant Asteroid Impact
- ↑ U.S. Geological Survey. "Iowa Meteorite Crater Confirmed". Retrieved 7 March 2013.
- ↑ Wu Siben. "Geologic feature of the Duolun impact crater".
- 1 2 Stephen Luntz. "Huge Asteroid Impact Identified".
- ↑ Amos, J (2009) 'Fried Egg' may be impact crater BBC News.
- ↑ R. Iaskty and A. Glikson (2005). "Gnargoo: a possible 75 km-diameter post-Early Permian – pre-Cretaceous buried impact structure, Carnarvon Basin, Western Australia", Australian Journal of Earth Sciences, Vol 52, 2005
- 1 2 Frank Dachille. "Frequency of the formation of large terrestrial impact craters".
- 1 2 Zeylik B. S.; Seytmuratova E. Yu, 1974: A meteorite-impact structure in central Kazakhstan and its magmatic-ore controlling role. Doklady Akademii Nauk SSSR: 1, Pages 167-170
- ↑ A. P. Crósta1, M.A.R. Vasconcelos (2013). Update On The Current Knowledge Of The Brazilian Impact Craters.
- ↑ Kenkmann, T., Afifi, A. M., Stewart, S. A., Poelchau, M. H., Cook, D. J. and Neville, A. S. (2015), Saqqar: A 34 km diameter impact structure in Saudi Arabia. Meteoritics & Planetary Science, 50: 1925–1940.
- ↑ A. P. Rossi; A. Baliva & E. Piluso (2003). "New Evidences of an Impact Origin for Temimichat Crater, Mauritania" (PDF). Lunar and Planetary Science (Lunar and Planetary Institute). XXXIV.
- ↑ G. Monegato; M. Massironi & E. Martellato (2010). "The Ring Structure of Wembo-Nyama (Eastern Kasai, R.D. Congo): A Possible Impact Crater in Central Africa" (PDF). Lunar and Planetary Science (Lunar and Planetary Institute) XLI.
- ↑ "Ring may be giant 'impact crater'". BBC News. 2010-03-10. Retrieved 2010-05-08.
- ↑ Vastag, Brian (18 February 2013). "Crater found in Iowa points to asteroid break-up 470 million years ago". Washington Post. Retrieved 19 February 2013.
- ↑ Double space strike 'caused dinosaur extinction' http://www.bbc.co.uk/news/science-environment-11112417
- ↑ Jolley D., Gilmour I., Gurov E., Kelley S., Watson J. (2010) Two large meteorite impacts at the Cretaceous-Paleogene boundary Geology September 2010, v. 38, pp. 835–838, doi:10.1130/G31034.1
- ↑ Ernstson, K., Claudin, F., Schüssler, U. & Hradil, K. (2002): The mid-Tertiary Azuara and Rubielos de la Cérida paired impact structures (Spain) - Treb. Mus. Geol. Barcelona, 11, 5 - 65.
- ↑ Becker L., Shukolyukov A., Macassic C., Lugmair G. & Poreda R. 2006. Extraterrestrial Chromium at the Graphite Peak P/Tr boundary and in the Bedout Impact Melt Breccia. Lunar and Planetary Science XXXVII (2006), abstract # 2321.PDF
- ↑ Gorder, Pam Frost (June 1, 2006). "Big Bang in Antarctica – Killer Crater Found Under Ice". Ohio State University Research News.
External links
- Earth Impact Database – List of confirmed earth impact sites at the Planetary and Space Science Centre, University of New Brunswick
- Impact Database (formerly Suspected Earth Impact Sites list) maintained by David Rajmon for Impact Field Studies Group, USA