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Impact events appear to have played a significant role in the evolution of the Solar System since its formation.
Major impact events have significantly shaped Earth's history , have been implicated in the formation of the Earth—Moon system , the evolutionary history of life , the origin of water on Earth and several mass extinctions. Notable impact events include the Chicxulub impact , 66 million years ago, believed to be the cause of the Cretaceous—Paleogene extinction event.
Throughout recorded history, hundreds of Earth impacts and exploding bolides have been reported, with some occurrences causing deaths, injuries, property damage, or other significant localised consequences. The Chelyabinsk meteor event is the only known such incident in modern times to result in a large number of injuries, excluding the Ch'ing-yang event in China.
The Chelyabinsk meteor is the largest recorded object to have encountered the Earth since the Tunguska event. The Comet Shoemaker—Levy 9 impact provided the first direct observation of an extraterrestrial collision of Solar System objects, when the comet broke apart and collided with Jupiter in July An extrasolar impact was observed in , when a massive terrestrial planet impact was detected around the star ID8 in the star cluster NGC by NASA's Spitzer space telescope and confirmed by ground observations.
In April , the B Foundation reported "It's a per cent certain we'll be hit [by a devastating asteroid], but we're not per cent sure when.
Major impact events have significantly shaped Earth's history , having been implicated in the formation of the Earth—Moon system , the evolutionary history of life , the origin of water on Earth , and several mass extinctions. Impact structures are the result of impact events on solid objects and, as the dominant landforms on many of the System's solid objects, present the most solid evidence of prehistoric events.
Notable impact events include the Late Heavy Bombardment , which occurred early in history of the Earth—Moon system, and the Chicxulub impact , 66 million years ago, believed to be the cause of the Cretaceous—Paleogene extinction event. Small objects frequently collide with Earth. There is an inverse relationship between the size of the object and the frequency of such events. The lunar cratering record shows that the frequency of impacts decreases as approximately the cube of the resulting crater's diameter, which is on average proportional to the diameter of the impactor.
The energy released by an impactor depends on diameter, density, velocity, and angle. The density is generally assumed because the diameter and mass are also generally estimates. Impact conditions such as asteroid size and speed, but also density and impact angle determine the kinetic energy released in an impact event. The more energy is released, the more damage is likely to occur on the ground due to the environmental effects triggered by the impact. Such effects can be shock waves, heat radiation, the formation of craters with associated earthquakes, and tsunamis if water bodies are hit.
Human populations are vulnerable to these effects if they live within the affected zone. The Chelyabinsk meteor was estimated to be about 20 m in diameter with an airburst of around kilotons, an explosion 30 times the one over Hiroshima.
Much larger objects may impact the solid earth and create a crater. An estimated meteorites reach the surface each year, but only 5 or 6 of these typically create a weather radar signature with a strewn field large enough to be recovered and be made known to scientists.
The late Eugene Shoemaker of the U. Geological Survey estimated the rate of Earth impacts, concluding that an event about the size of the nuclear weapon that destroyed Hiroshima occurs about once a year. Although no human is known to have been killed directly by an impact [ disputed — discuss ] , over people were injured by the Chelyabinsk meteor airburst event over Russia in Impacts have had, during the history of the Earth, a significant geological  and climatic  influence.
The Moon 's existence is widely attributed to a huge impact early in Earth's history. These modified views of Earth's history did not emerge until relatively recently, chiefly due to a lack of direct observations and the difficulty in recognizing the signs of an Earth impact because of erosion and weathering. Large-scale terrestrial impacts of the sort that produced the Barringer Crater , locally known as Meteor Crater , northeast of Flagstaff, Arizona, are rare.
Instead, it was widely thought that cratering was the result of volcanism: Similarly, the craters on the surface of the Moon were ascribed to volcanism. It was not until — that the Barringer Crater was correctly identified as an impact crater , and it was not until as recently as that research by Eugene Merle Shoemaker conclusively proved this hypothesis.
The findings of late 20th-century space exploration and the work of scientists such as Shoemaker demonstrated that impact cratering was by far the most widespread geological process at work on the Solar System's solid bodies.
Every surveyed solid body in the Solar System was found to be cratered, and there was no reason to believe that the Earth had somehow escaped bombardment from space.
In the last few decades of the 20th century, a large number of highly modified impact craters began to be identified. The first direct observation of a major impact event occurred in Only three confirmed craters from that time period with that size or greater have been found: Chicxulub , Popigai , and Manicouagan , and all three have been suspected of being linked to extinction events   though only Chicxulub, the largest of the three, has been consistently considered.
Besides direct effect of asteroid impacts on a planet's surface topography, global climate and life, recent studies have shown that several consecutive impacts might have an effect on the dynamo mechanism at a planet's core responsible for maintaining the magnetic field of the planet , and might eventually shut down the planet's magnetic field. While numerous impact craters have been confirmed on land or in the shallow seas over continental shelves , no impact craters in the deep ocean have been widely accepted by the scientific community.
The lack of a crater, however, does not mean that an ocean impact would not have dangerous implications for humanity. Some scholars have argued that an impact event in an ocean or sea may create a megatsunami a giant wave , which can cause destruction both at sea and on land along the coast,  but this is disputed.
An impact event may cause a mantle plume volcanism at the antipodal point of the impact. The effect of impact events on the biosphere has been the subject of scientific debate. Several theories of impact-related mass extinction have been developed. In the past million years there have been five generally accepted major mass extinctions that on average extinguished half of all species. There is no definitive evidence of impacts leading to the three other major mass extinctions. Michael from the University of California, Berkeley discovered unusually high concentrations of iridium in a specific layer of rock strata in the Earth's crust.
Iridium is an element that is rare on Earth but relatively abundant in many meteorites. This iridium layer at the Cretaceous—Paleogene boundary has been found worldwide at different sites. Multidirectionally shocked quartz coesite , which is normally associated with large impact events  or atomic bomb explosions, has also been found in the same layer at more than 30 sites. Soot and ash at levels tens of thousands times normal levels were found with the above. Anomalies in chromium isotopic ratios found within the K-T boundary layer strongly support the impact theory.
Further, the chromium isotopic ratios measured in the K-T boundary are similar to the chromium isotopic ratios found in carbonaceous chondrites. Thus a probable candidate for the impactor is a carbonaceous asteroid, but a comet is also possible because comets are assumed to consist of material similar to carbonaceous chondrites.
Probably the most convincing evidence for a worldwide catastrophe was the discovery of the crater which has since been named Chicxulub Crater. This convinced the vast majority of scientists that this extinction resulted from a point event that is most probably an extraterrestrial impact and not from increased volcanism and climate change which would spread its main effect over a much longer time period. Although there is now general agreement that there was a huge impact at the end of the Cretaceous that led to the iridium enrichment of the K-T boundary layer, remnants have been found of other, smaller impacts, some nearing half the size of the Chicxulub crater, which did not result in any mass extinctions, and there is no clear linkage between an impact and any other incident of mass extinction.
Raup and Jack Sepkoski have proposed that an excess of extinction events occurs roughly every 26 million years though many are relatively minor.
This led physicist Richard A. Muller to suggest that these extinctions could be due to a hypothetical companion star to the Sun called Nemesis periodically disrupting the orbits of comets in the Oort cloud , leading to a large increase in the number of comets reaching the inner Solar System where they might hit Earth.
Physicist Adrian Melott and paleontologist Richard Bambach have more recently verified the Raup and Sepkoski finding, but argue that it is not consistent with the characteristics expected of a Nemesis-style periodicity. An impact event is commonly seen as a scenario that would bring about the end of civilization. In , Discover Magazine published a list of 20 possible sudden doomsday scenarios with an impact event listed as the most likely to occur.
A majority 61 percent disagreed. In the early history of the Earth about four billion years ago , bolide impacts were almost certainly common since the Solar System contained far more discrete bodies than at present. Such impacts could have included strikes by asteroids hundreds of kilometers in diameter, with explosions so powerful that they vaporized all the Earth's oceans.
It was not until this heavy bombardment slackened that life appears to have begun to evolve on Earth. The leading theory of the Moon's origin is the giant impact theory , which postulates that Earth was once hit by a planetoid the size of Mars; such a theory is able to explain the size and composition of the Moon, something not done by other theories of lunar formation. Evidence of a massive impact in South Africa near a geological formation known as the Barberton Greenstone Belt was uncovered by scientists in April They estimated the impact occurred about 3.
The crater from this event, if it still exists, has not yet been found. Two kilometre sized asteroids are now believed to have struck Australia between and million years ago at the Western Warburton and East Warburton Basins creating a kilometre impact zone. According to evidence found in it is the largest ever recorded.
Artifacts recovered with tektites from the ,year-old Australasian strewnfield event in Asia link a Homo erectus population to a significant meteorite impact and its aftermath. The Rio Cuarto craters in Argentina were produced approximately 10, years ago, at the beginning of the Holocene. If proved to be impact craters, they would be the first impact of the holocene. The Campo del Cielo "Field of Heaven" refers to an area bordering Argentina's Chaco Province where a group of iron meteorites were found, estimated as dating to 4,—5, years ago.
It first came to attention of Spanish authorities in ; in , police arrested four alleged smugglers trying to steal more than a ton of protected meteorites. Whitecourt crater in Alberta, Canada is estimated to be between 1, and 1, years old.
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