List of possible impact structures on Earth
This is a list of possible impact structures on Earth. More than 130 features on Earth include candidate impact sites that have appeared several times in the literature and/or have been endorsed by the Impact Field Studies Group and/or Expert Database on Earth Impact Structures,. The Earth Impact Database is used at Wikipedia as authoritative using the terminology "confirmed". The list below includes a three-step confidence level as indicated by the Russian Academy of Sciences, by Anna Mikheeva: 1 for probable, 2 for potential, 3 for questionable. Level 4 is given to discredited structures, hence represent geological features other than impact craters. Structures with confidence 0 are considered "confirmed" or "proven" and should be placed in the lists per continent.
List of possible impact structures
The following tables list geological features on Earth that some individuals have associated with impact events, but for which there is currently no confirming scientific evidence in the peer-reviewed literature. In order for a structure to be a confirmed as an impact crater, it must meet a stringent set of well established criteria. Some proposed impact structures are eventually confirmed, whereas others are shown to be misidentified. Recent extensive surveys have been done for Australian, African, and South American craters, as well as those in the Arab world. A book review by A. Crósta and U. Reimold disputes some of the evidence presented for several of the South American structures.Confidence | 0 - proven |
Confidence | 1 – probable |
Confidence | 2 – potential |
Confidence | 3 – questionable |
Confidence | 4 – discredited |
Diameter | Kilometers |
Age | Approximate |
Name | Location | Confidence | Diameter | Age | Notes | Image | Coordinates |
38th Parallel structures | United States | variable | |||||
Ak-Bura | Tajikistan | 1 | 0.080 | ||||
Al Madafi | Saudi Arabia | 1 | 6 | ||||
Alamo bolide impact | United States | 0 | 367 | ||||
Anéfis | Mali | 2 | 3.9 | ||||
Aorounga Central | Chad | 0 | 11.6 | ||||
Arganaty | Kazakhstan | 0 | 300 | 250 | |||
Arlit | Niger | 2 | 10 | ? | |||
Australian impact structure | Australia | Highly speculative | 600 | ||||
Azuara | Spain | 1 | |||||
Bajada del Diablo | Argentina | 2 | 40 | ||||
Bajo Hondo | Argentina | 2 | 3.9 | ||||
Bangui magnetic anomaly | Central African Republic | 2 | |||||
Bateke Plateau | Gabon | 3 | 7.1 | ||||
Bedout | Australia | 2 | 250 | 250 | |||
Bee Bluff | United States | 0 | 2.4 | ||||
Björkö | Sweden | 1 | 10 | 1200 | |||
Bloody Creek | Canada | 1 | 40 | ? | |||
Bohemian crater | Czech Republic | 2 | |||||
Bow City | Canada | 2 | 8 | 70 | |||
Bowers crater | Antarctic Ocean | 2 | 100 | ||||
Brushy Creek Feature | United States | 1 | 2.0 | ||||
Burckle | Indian Ocean | 1 | |||||
Catalina structures | Pacific Ocean | 2 | |||||
Cerro do Jarau | Brazil | 1 | 10 | 117 | |||
Charity Shoal | Canada | 2 | 1.2 | ||||
Corossol | Canada | 3 | 4 | ||||
Darwin Crater | Tasmania | 0 | 1.2 | 0.816 | |||
Decorah | United States | 2 | 5.6 | 470 | |||
Diamantina River ring feature | Australia | 2 | 120 | 300 | |||
Dumas magnetic anomaly | Canada | 1 | 3.2 | ||||
Duolun | China | 2 | |||||
El-Baz | Egypt | 1 | 4 | ? | |||
Eltanin | Pacific Ocean | 0 | 2.5 | ||||
Faya Basin | Chad | 1 | 2 | ||||
Falkland Plateau anomaly | Atlantic Ocean | 2 | 250 | ||||
Fried Egg structure | Atlantic Ocean | 2 | 6 | 17 | |||
Garet El Lefet | Libya | 1 | 3 | ? | |||
Gatun structure | Panama | 1 | 3 | 20 | |||
General San Martín | Argentina | 2 | 11 | 1.2 | |||
Gnargoo | Australia | 1 | 75 | ||||
Guarda | Portugal | 1 | 30 | 200 | |||
Gulf of Mexico | United States, Mexico, Cuba | ||||||
Hartney anomaly | Canada | 1 | 8 | ||||
Hiawatha | Greenland | 2 | 31 | ||||
Hickman | Australia | 2 | 30 | ||||
Hico | United States | 1 | 9 | ||||
Hotchkiss | Canada | 1 | 4 | ||||
Howell | United States | 1 | 2.5 | ||||
Ibn-Batutah | Libya | 2 | 2.5 | ||||
Ishim | Kazakhstan | 0 | 300 | ||||
Iturralde | Bolivia | 1 | 8.0 | ||||
Jackpine Creek magnetic anomaly | Canada | 1 | 25 | ||||
Jebel Hadid | Libya | 2 | 4.7 | ||||
Jeptha Knob | United States | 0 | 4.3 | 425 | |||
Johnsonville | United States | 0 | 11 | ||||
Jwaneng South | Botswana | 2 | 1.3 | ||||
Luna | India | 2 | 2.1 | ||||
Kebira | Egypt | 2 | 31 | 100 | |||
Kilmichael | United States | 1 | 13 | 45 | |||
Krk structure | Croatia | 2 | 12 | 40 | |||
Kurai Basin | Russia | 1 | 20 | ||||
La Dulce | Argentina | 1 | 2.8 | ||||
Labynkyr | Russia | 0 | 67 | ||||
Lac Iro | Chad | 1 | 13 | ? | |||
Lairg Gravity Low | Scotland | 2 | 40 | 1200 | |||
Lake Cheko | Russia | 3 | 50 | ||||
Lake Tai | China | 1 | |||||
Loch Leven | Scotland | 2 | 290 | ||||
Lorne Basin | Australia | 2 | 30 | ||||
Lycksele structure 2 | Sweden | 2 | 130 | ||||
Madagascar structure 3 | Madagascar | 4 | 12 | ? | |||
Magyarmecske anomaly | Hungary | 1 | 7 | 299 | |||
Mahuika | New Zealand | 2 | |||||
Maniitsoq structure | Greenland | 2 | 100 | 3000 | |||
Mejaouda | Mauritania | 1 | 3 | ||||
Merewether | Canada | 0 | 20 | ||||
Meseta de la Barda Negra | Argentina | 4 | 1.5 | ||||
Middle-Urals Ring Structure | Russia | 1 | |||||
Mistassini-Otish impact structure | Canada | 1 | 600 | 2200 | |||
Mount Ashmore dome | Indian Ocean | 2 | 35 | ||||
Mousso | Chad | 2 | 3.8 | ||||
Mt. Oikeyama | Japan | 2 | 90 | ||||
Mulkarra | Australia | 1 | 17 | 105 | |||
Nastapoka arc | Canada | 3 | 450 | ||||
Ouro Ndia | Mali | 2 | 3 | ||||
Pantasma | Nicaragua | 3 | 10 | ? | |||
Panther Mountain | United States | 1 | 10 | 375 | |||
Peerless structure | United States | 1 | 6 | ||||
Piratininga | Brazil | 3 | 12 | 117 | |||
Praia Grande | Brazil | 1 | 20 | 84 | |||
Ramgarh | India | 0 | 3 | ? | |||
Ross | Antarctic Ocean | 2 | |||||
Rubielos de la Cérida | Spain | 0 | |||||
Sakhalinka | Pacific Ocean | 2 | 12 | 70 | |||
São Miguel do Tapuio | Brazil | 1 | 22 | 120 | |||
Shanghewan | China | 1 | 30 | ? | |||
Shiva | Indian Ocean | 1 | 500 | 66 | |||
Shiyli | Kazakhstan | 0 | 5.5 | ||||
Silverpit | Atlantic Ocean | 1 | 20 | ||||
Sirente | Italy | 4 | 10 | ||||
Sithylemenkat Lake | United States | 3 | 12 | ||||
Smerdyacheye Lake | Russia | 1 | 20 | ||||
Sudan 3 | Sudan | 2.8 | ? | ||||
Sudan 2 | Sudan | 2 | 10 | ? | |||
Sudan 1 | Sudan | 2 | 6 | ? | |||
Svetloyar Lake | Russia | 0 | 40 | ||||
Takamatsu | Japan | 1 | 15 | ||||
Tarek | Egypt | 3 | 2.1 | ||||
Tatarsky North | Pacific Ocean | 2 | 14 | ? | |||
Tatarsky South | Pacific Ocean | 2 | 20 | ? | |||
Tefé River structure | Brazil | 2 | 15 | ||||
Talundilly | Australia | 1 | 84 | ||||
Temimichat | Mauritania | 1 | 0.7 | ||||
Tsenkher | Mongolia | 1 | 3.6 | 5 | |||
Toms Canyon | United States | 1 | 22 | 35 | |||
Umm al Binni | Iraq | 0 | 3.4 | ||||
Ust-Kara | Russia | 2 | 25 | ||||
Vélingara | Senegal | 1 | 48 | ||||
Versailles | United States | 1 | 1.5 | ||||
Vichada | Colombia | 2 | 50 | ||||
Victoria Island | United States | 2 | 5.5 | ||||
Warburton East | Australia | 2 | 200 | ||||
Warburton West | Australia | 200 | |||||
Weaubleau | United States | 1 | 19 | ||||
Wembo-Nyama | DR Congo | 2 | |||||
Wilkes Land 2 | Antarctica | 2 | 480 | ||||
Woodbury | United States | 1 | 7 | ||||
Yallalie | Australia | 0 | 12 | ||||
Zerelia West | Greece | 2 | 20 | ||||
Zerelia East | Greece | 2 | 10 |
Overview
The Cheko crater is thought by one research group to be the result of the famous Tunguska event, although sediments in the lake have been dated back more than 5,000 years. There is highly speculative conjecture about the supposed Sirente impact causing the Roman emperor Constantine's vision at Milvian Bridge.The Burckle crater and Umm al Binni structure are proposed to be behind the floods that affected Sumerian civilization. The Kachchh impact may have been witnessed by the Harappan civilization and mentioned as a fireball in Sanskrit texts.
The ages of the Bloody Creek crater and Hiawatha crater are uncertain.
As the trend in the Earth Impact Database for about 26 confirmed craters younger than a million years old show that almost all are less than in diameter, the suggestion that two large craters, Mahuika and Burckle, formed just within the last few millennia has been met with skepticism.
However, the source of the young and enormous Australasian strewnfield is suggested to be a crater about across somewhere in Indochina, with Hartung and Koeberl proposing the elongated Tonlé Sap lake in Cambodia as a suspect structure.
The Decorah crater has been conjectured as being part of the Ordovician meteor event.
Several twin impacts have been proposed such as the Rubielos de la Cérida and Azuara, Cerro Jarau and Piratininga, and Warburton East and West. However, adjacent craters may not necessarily have formed at the same time such as case of the confirmed Clearwater East and West lakes.
Some confirmed impacts like Sudbury or Chicxulub are also sources of magnetic anomalies and/or gravity anomalies. The magnetic anomalies Bangui and Jackpine Creek, the gravity anomalies Wilkes Land crater and Falkland Islands, and others have been considered as being of impact origin. Bangui apparently has been discredited, but appears again in a 2014 table of unconfirmed structures in Africa by Reimold and Koeberl.
Several anomalies in Williston Basin were identified by Swatzky in the 1970s as astroblemes including Viewfield, Red Wing Creek, Eagle Butte, Dumas, and Hartney, of which only the last two are unconfirmed.
The Eltanin impact has been confirmed but, as it fell into the Pacific Ocean, apparently no crater was formed. The age of Silverpit and the confirmed Boltysh crater, as well as their latitude, has led to the speculative hypothesis that there may have been several impacts during the KT boundary. Of the five oceans in descending order by area, namely the Pacific, Atlantic, Indian, Antarctic, and Arctic, only the smallest does not yet have a proposed unconfirmed impact crater.
Craters larger than in the Phanerozoic 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 is conjectured to be bounded by the late Ordivician-early Silurian, the two Warburton basins have been linked to the Late Devonian extinction, both Bedout and the Wilkes Land crater have been associated with the severe Permian–Triassic extinction event, Manicouagan was once thought to be connected to the Triassic–Jurassic extinction event but more recent dating has made it unlikely, while the consensus is the Chicxulub impact caused the one for Cretaceous–Paleogene.
However, other extinction theories employ coeval periods of massive volcanism such as the Siberian Traps and Deccan Traps.
Undiscovered but inferred
There is geological evidence for impact events having taken place on Earth on certain specific occasions, which should have formed craters, but for which no impact craters have been found. In some cases this is because of erosion and Earth's crust having been recycled through plate tectonics, in others likely because exploration of the Earth's surface is incomplete. Typically the ages are already known and the diameters can be estimated.Parent crater of | Expected crater diameter | Age | Notes |
Dakhleh glass | 0.4 km | 150 ka | |
Argentinian tektites | 5 km | 480 ka | |
Australasian tektites | 32–114 km | 780 ka | |
Central American tektites | 14 km | 820 ka | |
Skye ejecta deposits | Unknown | 60 Ma | |
Stac Fada Member | 40 km | 1.2 Ga | |
Barberton Greenstone Belt microtektites | 500 km | 3.2 Ga | |
Marble Bar impact spherules | "hundreds of kilometers" | 3.4 Ga |
Mistaken identity
Some geological processes can result in circular or near-circular features that may be mistaken for impact craters. Some examples are calderas, maars, sinkholes, glacial cirques, igneous intrusions, ring dikes, salt domes, geologic domes, ventifacts, tuff rings, forest rings, and others. Conversely, an impact crater may originally be thought as one of these geological features, like Meteor Crater or Upheaval Dome.The presence of shock metamorphism and shatter cones are important criteria in favor of an impact interpretation, though massive landslides may produce shock-like fused rocks called "frictionite".