An impact event is a collision between celestial objects causing measurable effects. Impact events have physical consequences and have been found to regularly occur in planetary systems, though the most frequent involve asteroids, comets or meteoroids and have minimal impact. When large objects impact terrestrial planets like the Earth, there can be significant physical and biospheric consequences, though atmospheres mitigate many surface impacts through atmospheric entry. Impact structures are dominant landforms on many of the System's solid objects and present the strongest empirical evidence for their frequency and scale.
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 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.
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. One of the best-known recorded impacts in modern times was the Tunguska event, which occurred in Siberia, Russia, in 1908. The 2013 Chelyabinsk meteor event is the only known such event to result in a large number of injuries, and the Chelyabinsk meteor is the largest recorded object to have encountered the Earth since the Tunguska event.
The most notable non-terrestrial event is the Comet Shoemaker–Levy 9 impact, which provided the first direct observation of an extraterrestrial collision of Solar System objects, when the comet broke apart and collided with Jupiter in July 1994. Most of the observed extrasolar impacts are the slow collision of galaxies, however in 2014, one of the first massive terrestrial impacts observed was detected around the star NGC 2547 by NASA's Spitzer space telescope and confirmed by ground observations. Impact events have been a plot and background element in science fiction.
- 1 Impacts and the Earth
- 2 Elsewhere in the Solar Systems
- 3 Extrasolar impacts
- 4 Popular culture
- 5 See also
- 6 References
- 7 Further reading
- 8 External links
Impacts and the Earth
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. 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.
Frequency and risk
|“||REP. STEWART: ... are we technologically capable of launching something that could intercept [an asteroid]? ... DR. A'HEARN: No. If we had spacecraft plans on the books already, that would take a year ... I mean a typical small mission ... takes four years from approval to start to launch ...||”|
Small objects frequently collide with Earth. There is an inverse relationship between the size of the object and the frequency that such objects hit Earth. 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. Asteroids with a 1 km (0.62 mi) diameter strike Earth every 500,000 years on average. Large collisions – with 5 km (3 mi) objects – happen approximately once every twenty million years. The last known impact of an object of 10 km (6 mi) or more in diameter was at the Cretaceous–Paleogene extinction event 66 million years ago.
The energy released by an impactor depends on diameter, density, velocity, and angle. The diameter of most near-Earth asteroids that have not been studied by radar or infrared can generally only be estimated within about a factor of 2 based on the asteroid brightness. The density is generally assumed because the diameter and mass are also generally estimates. The minimum impact velocity on Earth is 11 km/s with asteroid impacts averaging around 17 km/s. The most probable impact angle is 45 degrees.
Stony asteroids with a diameter of 4 meters (13 ft) impact Earth approximately once per year. Asteroids with a diameter of 7 meters enter Earth's atmosphere with as much kinetic energy as Little Boy (the atomic bomb dropped on Hiroshima, approximately 16 kilotons of TNT) about every 5 years, but the air burst only generates a much reduced 5 kilotons of TNT. These ordinarily explode in the upper atmosphere, and most or all of the solids are vaporized. Objects with a diameter of roughly 50 m (164 ft) strike Earth approximately once every thousand years, producing explosions comparable to the one known to have detonated roughly 8.5 kilometers (28,000 ft) above Tunguska in 1908.
|Kinetic energy at
|100 m (330 ft)||47 Mt||38 Mt||1.2 km (0.75 mi)||5200 years|
|130 m (430 ft)||103 Mt||64.8 Mt||2 km (1.2 mi)||11000 years|
|150 m (490 ft)||159 Mt||71.5 Mt||2.4 km (1.5 mi)||16000 years|
|200 m (660 ft)||376 Mt||261 Mt||3 km (1.9 mi)||36000 years|
|250 m (820 ft)||734 Mt||598 Mt||3.8 km (2.4 mi)||59000 years|
|300 m (980 ft)||1270 Mt||1110 Mt||4.6 km (2.9 mi)||73000 years|
|400 m (1,300 ft)||3010 Mt||2800 Mt||6 km (3.7 mi)||100000 years|
|700 m (2,300 ft)||16100 Mt||15700 Mt||10 km (6.2 mi)||190000 years|
|1,000 m (3,300 ft)||47000 Mt||46300 Mt||13.6 km (8.5 mi)||440000 years|
|Kinetic energy at
|4 m (13 ft)||3 kt||0.75 kt||42.5 km (139,000 ft)||1.3 years|
|7 m (23 ft)||16 kt||5 kt||36.3 km (119,000 ft)||4.6 years|
|10 m (33 ft)||47 kt||19 kt||31.9 km (105,000 ft)||10.4 years|
|15 m (49 ft)||159 kt||82 kt||26.4 km (87,000 ft)||27 years|
|20 m (66 ft)||376 kt||230 kt||22.4 km (73,000 ft)||60 years|
|30 m (98 ft)||1.3 Mt||930 kt||16.5 km (54,000 ft)||185 years|
|50 m (160 ft)||5.9 Mt||5.2 Mt||8.7 km (29,000 ft)||764 years|
|70 m (230 ft)||16 Mt||15.2 Mt||3.6 km (12,000 ft)||1900 years|
|85 m (279 ft)||29 Mt||28 Mt||0.58 km (1,900 ft)||3300 years|
(The tables above use a density of 2600 kg/m3, velocity of 17 km/s, and an angle of 45 degrees)
Objects with a diameter less than 1 m (3.3 ft) are called meteoroids and seldom make it to the ground to become meteorites. An estimated 500 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.S. Geological Survey estimated of the rate of Earth impacts, concluding that an event about the size of the nuclear weapon that destroyed Hiroshima occurs about once a year. Such events would seem to be spectacularly obvious, but they generally go unnoticed for a number of reasons: the majority of the Earth's surface is covered by water; a good portion of the land surface is uninhabited; and the explosions generally occur at relatively high altitude, resulting in a huge flash and thunderclap but no real damage.
Although no human is known to have been killed directly by an impact, over one thousand people were injured by the Chelyabinsk meteor airburst event over Russia in 2013. In 2005 it was estimated that the chance of a single person born today dying due to an impact is around 1 in 200 000. The 4-meter-sized asteroids 2008 TC3 and 2014 AA are the only known objects to be detected before impacting the Earth.
The Moon is widely attributed to a huge impact early in Earth's history. Impact events earlier in the history of Earth have been credited with creative as well as destructive events; it has been proposed that impacting comets delivered the Earth's water, and some have suggested that the origins of life may have been influenced by impacting objects by bringing organic chemicals or lifeforms to the Earth's surface, a theory known as exogenesis.
These modified views of the 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: the Barringer Crater, for example, was ascribed to a prehistoric volcanic explosion (not an unreasonable hypothesis, given that the volcanic San Francisco Peaks stand only 30 miles (48 km) to the west). Similarly, the craters on the surface of the Moon were ascribed to volcanism.
It was not until 1903–1905 that the Barringer Crater was correctly identified as being an impact crater, and it was not until as recently as 1963 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 twentieth century, a large number of highly modified impact craters began to be identified. The largest of these include Vredefort Crater, Sudbury Crater, Chicxulub Crater, and Manicouagan Crater. The first observation of a major impact event occurred in 1994: the collision of the comet Shoemaker-Levy 9 with Jupiter; to date, no such events have been observed on Earth.
Based on crater formation rates determined from the Earth's closest celestial partner, the Moon, astrogeologists have determined that during the last 600 million years, the Earth has been struck by 60 objects of a diameter of 5 km (3 mi) or more. The smallest of these impactors would release the equivalent of ten million megatons of TNT and leave a crater 95 km (60 mi) across. For comparison, the largest nuclear weapon ever detonated, the Tsar Bomba, had a yield of 50 megatons.
Besides direct effect of asteroid impacts on a planet's surface topography, global climate and life, recent studies have shown that several consecutive impacts can have effect on the dynamo mechanism at a planet's core responsible for maintaining the magnetic field of the planet, and can 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. Impacts of projectiles as large as 1 km in diameter are generally thought to explode before reaching the sea floor, but it is unknown what would happen if a much larger impactor struck the deep ocean. 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.
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 500 million years there have been five generally accepted, major mass extinctions that on average extinguished half of all species. One of the largest mass extinction to have affected life on Earth was in the Permian-Triassic, which ended the Permian period 250 million years ago and killed off 90% of all species; life on Earth took 30 million years to recover. The cause of the Permian-Triassic extinction is still matter of debate with the age and origin of proposed impact craters, i.e. the Bedout High structure, hypothesized to be associated with it are still controversial. The last such mass extinction led to the demise of the dinosaurs and coincided with a large meteorite impact; this is the Cretaceous–Paleogene extinction event (also known as the K–T or K–Pg extinction event); This occurred 66 million years ago. There is no definitive evidence of impacts leading to the three other major mass extinctions.
In 1980, physicist Luis Alvarez; his son, geologist Walter Alvarez; and nuclear chemists Frank Asaro and Helen V. 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. From the amount and distribution of iridium present in the 65-million-year-old "iridium layer", the Alvarez team later estimated that an asteroid of 10 to 14 km (6 to 9 mi) must have collided with the earth. This iridium layer at the Cretaceous–Paleogene boundary has been found worldwide at 100 different sites. Multidirectionally shocked quartz (coesite), which is only known to form as the result of large impacts 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. Chromium isotopic ratios are homogeneous within the earth, therefore these isotopic anomalies exclude a volcanic origin which was also proposed as a cause for the iridium enrichment. Furthermore 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 also a comet is 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 crater is centered on the Yucatán Peninsula of Mexico and was discovered by Tony Camargo and Glen Pentfield while working as geophysicists for the Mexican oil company PEMEX. What they reported as a circular feature later turned out to be a crater estimated to be 180 km (110 mi) in diameter. Other researchers would later find that the end-Cretaceous extinction event that wiped out the dinosaurs had lasted for thousands of years instead of millions of years as had previously been thought. 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).
Recently, several proposed craters around the world have been dated to approximately the same age as Chicxulub — for example, the Silverpit crater in the United Kingdom, the Boltysh crater in Ukraine and the Shiva crater near India. This has led to the suggestion that the Chicxulub impact was one of several that occurred almost simultaneously, perhaps due to a disrupted comet impacting the Earth in a similar manner to the collision of Comet Shoemaker-Levy 9 with Jupiter in 1994; however, the uncertain age and provenance of these structures leaves the hypothesis without widespread support.
It was the lack of high concentrations of iridium and shocked quartz which has prevented the acceptance of the idea that the Permian extinction was also caused by an impact. During the late Permian all the continents were combined into one supercontinent named Pangaea and all the oceans formed one superocean, Panthalassa. If an impact occurred in the ocean and not on land at all, then there would be little shocked quartz released (since oceanic crust has relatively little silica) and much less material.
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.
Paleontologists David M. 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, and 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.
Sociological and cultural effects
An impact event is commonly seen as a scenario that would bring about the end of civilization. In 2000, Discover Magazine published a list of 20 possible sudden doomsday scenarios with an impact event listed as the most likely to occur.
Early Earth impacts
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.
In April 2014, scientists reported finding evidence of the largest impact event to date in South Africa near a geological formation known as the Barberton Greenstone Belt. They estimated the impact occurred about 3.26 billion years ago and that the impactor was approximately 37–58 kilometers (23–36 miles) wide. The crater from this event, if it still exists, has not yet been found.
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. Similar (but scaled down) impacts are commonly postulated as the origin of Pluto's large moon Charon, the Juno surviving planet Ceres, and Haumea's two large moons.
Artefacts recovered with tektites from the 803,000 year-old Australasian strewnfield event in Asia link a Homo Erectus population to a significant meteorite impact and its aftermath. Significant examples of Pleistocene impacts include the Rio Cuarto craters in Argentina, produced by an asteroid striking Earth at a very low angle, ~10,000 years old and the Lonar crater lake in India, which now has a flourishing semi-tropical jungle around it, ~52,000 years old (though a study published in 2010 gives a much greater age).
The Younger Dryas impact event is a contested hypothesis that an air burst from a purported comet above or even into the Laurentide Ice Sheet north of the Great Lakes set all of the North American continent ablaze around 12,900 years ago. The hypothesis attempts to explain the extinction of many of the large animals in North America and the unproven population decreases in the North American stone age Clovis culture about at the end of the Pleistocene epoch. Proponents claim the existence of a charred carbon-rich layer of soil found at some 50 Clovis-age sites across the continent. It has been criticized for not being consistent with paleoindian population estimates. Impact specialists have studied the claim and concluded that there never was such an impact, in particular because various physical signs of such an impact cannot be found. Evidence supporting the theory however has been further suggested by the 2012 paper presented to the PNAS (T.E. Bunch et al.) which looked at apparent high temperature impact melt products found in multiple sites of the 'black mat' across three continents dating to 12,900 years ago. This is further indicated by the discovery (Kurbatov et al. 2010) of the presence of a rich layer of nanodiamonds in the Greenland ice sheet coinciding with this date.
More recent prehistoric impacts are theorized by the Holocene Impact Working Group, including Dallas Abbott of Columbia University's Lamont-Doherty Earth Observatory. This group points to four enormous chevron sediment deposits at the southern end of Madagascar, containing deep-ocean microfossils fused with metals typically formed by cosmic impacts. All of the chevrons point toward a spot in the middle of the Indian Ocean corresponding with the newly hypothesized Burckle crater proposed to be some 29 km (18 mi) in diameter, or about 25 times larger than Barringer Crater. This group posits that a large asteroid or comet impact c. 2800-3000 BCE produced a mega-tsunami at least 180 m (590 ft) high, a catastrophic event that would have affected humanity's cradles of civilization. The evidence for the proposed crater has been challenged.
A Chinese record states that 10,000 people were killed in Shanxi Province in 1490 by a hail of "falling stones"; some astronomers hypothesize that this may describe the breakup of a large asteroid, although they find the number of deaths implausible.
Kamil Crater, discovered from Google Earth image review in Egypt, 45 m (148 ft) in diameter, 10 m (33 ft) deep is thought to have been formed less than 3,500 years ago in a then-unpopulated region of Western Egypt. It was found February 19, 2009 by V. de Michelle on a Google Earth image of the East Uweinat Desert, Egypt.
The Mahuika crater may have resulted from a modern impact event. The crater is located south of the Snares Islands (120 km (70 mi) southwest of Stewart Island) on the southern New Zealand shelf and is approximately 20 kilometers (12 mi) wide. Material extracted from Siple Dome ice core melt water indicates that the impact occurred around 1443 C.E.
Presumed impact events during 533–534 ± 2 CE have been proposed by the dendrochronologist Mike Baillie as a possible cause of several brief (typically 5-10 year) climatic downturns recorded in ancient tree ring patterns. Baillie highlights four such events and suggests that these might have been caused by the dust veils thrown up by the impact of cometary debris.
One of the best-known recorded impacts in modern times was the Tunguska event, which occurred in Siberia, Russia, in 1908. This incident involved an explosion that was probably caused by the airburst of an asteroid or comet 5 to 10 km (3.1 to 6.2 mi) above the Earth's surface, felling an estimated 80 million trees over 2,150 km2 (830 sq mi).
The first known modern strike to a human was on the April 28, 1927 in Aba, Japan, to the head of the five-year-old daughter of Mrs. Kuriyama; a bean-sized stone was found resting on her headband and now resides in a museum, called the Aba stone. The girl recovered several days later.
The first known modern case of a human injured by a space rock occurred on November 30, 1954, in Sylacauga, Alabama. There a 4 kg (8.8 lb) stone chondrite crashed through a roof and hit Ann Hodges in her living room after it bounced off her radio. She was badly bruised. Several persons have since claimed to have been struck by 'meteorites' but no verifiable meteorites have resulted.
A small number of meteor falls have been observed with automated cameras and recovered following calculation of the impact point. The first of these was the Přibram meteorite, which fell in Czechoslovakia (now the Czech Republic) in 1959. In this case, two cameras used to photograph meteors captured images of the fireball. The images were used both to determine the location of the stones on the ground and, more significantly, to calculate for the first time an accurate orbit for a recovered meteorite.
Following the Pribram fall, other nations established automated observing programs aimed at studying infalling meteorites. One of these was the Prairie Network, operated by the Smithsonian Astrophysical Observatory from 1963 to 1975 in the midwestern US. This program also observed a meteorite fall, the Lost City chondrite, allowing its recovery and a calculation of its orbit. Another program in Canada, the Meteorite Observation and Recovery Project, ran from 1971 to 1985. It too recovered a single meteorite, Innisfree, in 1977. Finally, observations by the European Fireball Network, a descendant of the original Czech program that recovered Pribram, led to the discovery and orbit calculations for the Neuschwanstein meteorite in 2002.
On August 10, 1972, a meteor which became known as the 1972 Great Daylight Fireball was witnessed by many people moving north over the Rocky Mountains from the U.S. Southwest to Canada. It was filmed by a tourist at the Grand Teton National Park in Wyoming with an 8-millimeter color movie camera. The object was in the range of size from a car to a house and could have ended its life in a Hiroshima-sized blast, but there was never any explosion. Analysis of the trajectory indicated that it never came much lower than 58 km (36 mi) off the ground, and the conclusion was that it had grazed Earth's atmosphere for about 100 seconds, then skipped back out of the atmosphere to return to its orbit around the Sun.
Many impact events occur without being observed by anyone on the ground. Between 1975 and 1992, American missile early warning satellites picked up 136 major explosions in the upper atmosphere. In the November 21, 2002, edition of the journal Nature, Peter Brown of the University of Western Ontario reported on his study of U.S. early warning satellite records for the preceding 8 years. He identified 300 flashes caused by 1 to 10 m (3 to 33 ft) sized meteors in that time period and estimated the rate of Tunguska-sized events as once in 400 years. Eugene Shoemaker estimated that one of such magnitude occurs about once every 300 years, though more recent analyses have suggested he exaggerated by an order of magnitude.
In the dark morning hours of January 18, 2000, a fireball exploded over the city of Whitehorse in the Canadian Yukon at an altitude of about 26 km (16 mi), lighting up the night like day. The meteor that produced the fireball was estimated to be about 4.6 m (15 ft) in diameter and with a weight of 180 tonnes. This blast was also featured on The Science Channel series Killer Asteroids, with several witness reports from residents in Atlin, British Columbia.
Comet Shoemaker–Levy 9 was a comet that broke apart and collided with Jupiter in July 1994, providing the first direct observation of an extraterrestrial collision of Solar System objects. In recent years, scientists have observed more Jupiter impact events (See 2009 Jupiter impact event and 2010 Jupiter impact event).
A meteor was observed striking Reisadalen in Nordreisa municipality in Troms County, Norway, on June 7, 2006. Although initial witness reports stated that the resultant fireball was equivalent to the Hiroshima nuclear explosion, scientific analysis places the force of the blast at anywhere from 100-500 tonnes TNT equivalent – around 3% of Hiroshima's yield.
On September 15, 2007, a chondritic meteor crashed near the village of Carancas in southeastern Peru near Lake Titicaca, leaving a water-filled hole and spewing gases across the surrounding area. Many residents became ill, apparently from the noxious gases shortly after the impact.
On October 7, 2008, a meteroid labeled 2008 TC3 was tracked for 20 hours as it approached Earth and as it fell through the atmosphere and impacted in Sudan. This was the first time an object was detected before it reached the atmosphere and hundreds of pieces of the meteorite were recovered from the Nubian Desert.
On November 21, 2009, a fireball was sighted in South Africa by police and traffic cameras. The probable meteor may have landed in a remote area on the Botswana border, and likely made little impact.
On February 15, 2013, an asteroid entered Earth's atmosphere over Russia as a fireball and exploded above the city of Chelyabinsk during its passage through the Ural Mountains region at 09:13 YEKT (03:13 UTC). The object's air burst occurred at an altitude between 30 and 50 km (19 and 31 mi) above the ground, and about 1,500 people were injured, mainly by broken window glass shattered by the shock wave. Two were reported in serious condition; however, there were no fatalities. Initially some 3,000 buildings in six cities across the region were reported damaged due to the explosion's shock wave, a figure which rose to over 7,200 in the following weeks. The Chelyabinsk meteor was estimated to have caused over $30 million in damages. It is the largest recorded object to have encountered the Earth since the 1908 Tunguska event, by far the best documented, and the only such event known to have resulted in a large number of casualties. The meteor is estimated to have an initial diameter of 17-20 metre and a mass of roughly 10,000 tonnes. On 16 October 2013, a team from Ural Federal University led by Victor Grokhovsky recovered a large fragment of the meteor from the bottom of Russia’s Lake Chebarkul, about 80 km west of the city.
Elsewhere in the Solar Systems
Evidence of massive past impact events
Impact craters provide evidence of past impacts on other planets in the Solar System, including possible interplanetary terrestrial impacts. Without carbon dating, other points of reference are used to estimate the timing of these impact events. Mars provides some significant evidence of possible interplanetary collisions. The North Polar Basin on Mars is speculated by some to be evidence for a planet sized impact on the surface of Mars between 3.8 and 3.9 billion years ago, while Utopia Planitia is the largest confirmed impact and Hellas Planitia is the largest visible crater in the Solar System. The Moon provides similar evidence of massive impacts, with the South Pole–Aitken basin being the biggest. Mercury's Caloris Basin is another example of a crater formed by a massive impact event. Rheasilvia on Vesta is an example of a crater formed by an impact capable of, based on ratio of impact to size, severely deforming a planetary-mass object. Impact craters on the moons of Saturn such as Engelier and Gerin on Iapetus, Mamaldi on Rhea and Odysseus on Tethys and Herschel on Mimas form significant surface features.
The 1994 impact of Comet Shoemaker-Levy 9 with Jupiter served as a "wake-up call", and astronomers responded by starting programs such as Lincoln Near-Earth Asteroid Research (LINEAR), Near-Earth Asteroid Tracking (NEAT), Lowell Observatory Near-Earth Object Search (LONEOS) and several others which have drastically increased the rate of asteroid discovery.
In 1998, two comets were observed plunging toward the Sun in close succession. The first of these was on June 1 and the second the next day. A video of this, followed by a dramatic ejection of solar gas (unrelated to the impacts), can be found at the NASA website. Both of these comets evaporated before coming into contact with the surface of the Sun. According to a theory by NASA Jet Propulsion Laboratory scientist Zdeněk Sekanina, the latest impactor to actually make contact with the Sun was the "supercomet" Howard-Koomen-Michels on August 30, 1979. (See also sungrazer.)
On July 19, 2009, a new black spot about the size of Earth was discovered in Jupiter's southern hemisphere by an amateur astronomer. Thermal infrared analysis showed it was warm and spectroscopic methods detected ammonia. JPL scientists confirmed that another impact event on Jupiter had occurred, probably a small undiscovered comet or other icy body.
NASA has actively monitored lunar impacts since 2005, tracking hundreds of candidate events. On March 19, 2013, an impact occurred that was visible from Earth, when a boulder sized 30 cm meteoroid slammed into the moon at 56,000 mph creating a 20 meter crater. Images from the Mars Reconnaissance Orbiter provide compelling evidence of the largest to date observed impact on Mars in the form of fresh impact craters, the largest measuring 48.5 by 43.5 meters. The impact is estimated to have occurred 27-28 March 2012 and caused by an impactor 3 to 5 meters long.
Collisions between galaxies, or galaxy mergers have been observed directly by space telescopes such as Hubble and Spitzer. However collisions in planetary systems including stellar collisions, while long speculated, have only recently begun to be observed directly.
In 2013, one of the first massive terrestrial impacts observed was detected around the star NGC 2547 by Spitzer and confirmed by ground observations. Computer modelling suggests that the impact involved large asteroids or protoplanets similar to the events believed to have led to the formation of terrestrial planets like the Earth.
Science fiction novels
Numerous science fiction stories and novels center around an impact event; one of the first and more popular being Off on a Comet (French: Hector Servadac) by Jules Verne, published in 1877. In more modern times possibly the best-selling was the novel Lucifer's Hammer by Larry Niven and Jerry Pournelle. Arthur C. Clarke's novel Rendezvous with Rama opens with a significant asteroid impact in northern Italy in the year 2077 which gives rise to the Spaceguard Project, which later discovers the Rama spacecraft. In 1992 a Congressional study in the U.S. led to NASA being directed to undertake a Spaceguard Survey, with the novel being named as the inspiration for the name to search for Earth-impacting asteroids. This in turn inspired Clarke's 1993 novel The Hammer of God.
A variation on the traditional impact story was provided by Jack McDevitt's 1999 novel Moonfall, in which a very large comet traveling at interstellar velocities collides with and partially destroys the Moon, fragments of which then collide with the Earth. The 1985 Niven and Pournelle novel Footfall features the examination of the effects of planetary warfare conducted by an alien species that culminates in the use of asteroids to bombard the planet, creating very large craters and the human species' near extinction. Robert A. Heinlein used the concept of guided meteors in his novel The Moon is a Harsh Mistress, in which the moon rebels use rock-filled shipping containers as a weapon against their Earth oppressors.
Some science fiction has concerned itself not with the specifics of the impact event and/or its prevention or avoidance but its secondary effects on human society. Ben H. Winters' 2012 novel The Last Policeman is set six months prior to an asteroid collision, following a murder investigation that is complicated by the political and cultural responses to the impending event.
Cinema and television
Several disaster films have also been made: released during the turbulence of World War I, the Danish feature film The End of the World revolves around the near-miss of a comet which causes fire showers and social unrest in Europe. When Worlds Collide (1951) based on a 1933 novel by Philip Wylie, deals with two planets on a collision course with Earth – the smaller planet a "near miss," causing extensive damage and destruction, followed by a direct hit from the larger planet. Meteor (1979) features small asteroid fragments and a large 8 km (5 mi) wide asteroid heading for Earth. Orbiting U.S. and Soviet nuclear weapons platforms are turned away from their respective earthbound targets, and toward the incoming threat.
In 1998, two films were released in the United States on the subject of attempting to stop impact events: Touchstone Pictures' Armageddon, about an asteroid; and Paramount/DreamWorks' Deep Impact, about a comet. Both involved using Space Shuttle-derived craft to deliver large amounts of nuclear weapons to destroy their targets. The 2008 American Broadcasting Company's miniseries Impact deals about a splinter of a brown dwarf hidden in a meteor shower which strikes the Moon and sends it on a collision course with Earth. The 2011 film Melancholia uses the motif of an impact event incorporated in the aesthetics of Romanticism.
In the science fiction television series Babylon 5, war between the Narn and Centauri is brought to an end when the Centauri use mass drivers to propel asteroids at the surface of the Narn home world causing severe ecological damage. The novelization, as well as the actual game Rage, is based on an alternate future, where the end of the world is caused by impact with 99942 Apophis.
- Asteroid capture
- Asteroid deflection strategies
- Near Earth Object Camera
- B612 Foundation
- Earth Impact Database
- Impact gardening
- Near-Earth asteroids
- Near-Earth objects
- Global catastrophic risks
- Potentially hazardous asteroid
- Torino scale, 0 to 10
- Palermo scale
- List of meteor air bursts
- List of impact craters on Earth
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|Wikimedia Commons has media related to Impact events.|
- Asteroid impacts on Earth: Skyfalls, The Economist, 26 April 2014.
- EARTH IMPACTS from Greg Goebel's IN THE PUBLIC DOMAIN
- Earth Impact Database
- Earth Impact Effects Program
- Nature journal video discussing historical impact event on Mars
- Impact Structure (Crater) Explorations
- All 172 confirmed meteor impact sites on earth, viewable in Google Earth (Largest, Most recent, Per continent, Including size indicator)
- Impact Meteor Crater Viewer Google Maps Page with Locations of Meteor Craters around the world
- Reorienting Western Society to Battle Impact Events Jagiellonian University, Poland
- A comet or asteroid impact with the earth - How real is the threat? Bob Hawkes
- arguing for a globally cooperative Earth Defense Initiative (EDI)
- Traces of Catastrophe
- GEOSIM - Information on impact processes and effects; 3-D-simulation
- Down 2 Earth Impact Calculator Interactive simulator showing size of craters on Google Maps
- Impact Site Map Interactive map, with simple html drilldowns to Google satellite maps of impact sites.
- Judson L. Ahern, Univ. of Okla.: DETECTING BURIED IMPACT STRUCTURES: EARTH AND MARS - general interest article
- Asteroid Impactor Reported over Indonesia
- R. Marcus, H. J. Melosh, and G. Collins. Earth Impact Effects Program, an online calculator for qualitative estimation of impact effects. Purdue University, Imperial College London.