An earthquake (also known as a quake, tremor or temblor) is the result of a sudden release of energy in the Earth's crust that creates seismic waves. The seismicity or seismic activity of an area refers to the frequency, type and size of earthquakes experienced over a period of time. Earthquakes are measured using observations from seismometers. The moment magnitude is the most common scale on which earthquakes larger than approximately 5 are reported for the entire globe. The more numerous earthquakes smaller than magnitude 5 reported by national seismological observatories are measured mostly on the local magnitude scale, also referred to as the Richter scale. These two scales are numerically similar over their range of validity. Magnitude 3 or lower earthquakes are mostly almost imperceptible and magnitude 7 and over potentially cause serious damage over large areas, depending on their depth. The largest earthquakes in historic times have been of magnitude slightly over 9, although there is no limit to the possible magnitude. The most recent large earthquake of magnitude 9.0 or larger was a 9.0 magnitude earthquake in Japan in 2011 (as of March 2011), and it was the largest Japanese earthquake since records began. Intensity of shaking is measured on the modified Mercalli scale. The shallower an earthquake, the more damage to structures it causes, all else being equal.

At the Earth's surface, earthquakes manifest themselves by shaking and sometimes displacement of the ground. When the epicenter of a large earthquake is located offshore, the seabed may be displaced sufficiently to cause a tsunami. Earthquakes can also trigger landslides, and occasionally volcanic activity.

In its most general sense, the word ''earthquake'' is used to describe any seismic event — whether natural or caused by humans — that generates seismic waves. Earthquakes are caused mostly by rupture of geological faults, but also by other events such as volcanic activity, landslides, mine blasts, and nuclear tests. An earthquake's point of initial rupture is called its focus or hypocenter. The epicenter is the point at ground level directly above the hypocenter.

Naturally occurring earthquakes

Tectonic earthquakes occur anywhere in the earth where there is sufficient stored elastic strain energy to drive fracture propagation along a fault plane. The sides of a fault move past each other smoothly and aseismically only if there are no irregularities or asperities along the fault surface that increase the frictional resistance. Most fault surfaces do have such asperities and this leads to a form of stick-slip behaviour. Once the fault has locked, continued relative motion between the plates leads to increasing stress and therefore, stored strain energy in the volume around the fault surface. This continues until the stress has risen sufficiently to break through the asperity, suddenly allowing sliding over the locked portion of the fault, releasing the stored energy. This energy is released as a combination of radiated elastic strain seismic waves, frictional heating of the fault surface, and cracking of the rock, thus causing an earthquake. This process of gradual build-up of strain and stress punctuated by occasional sudden earthquake failure is referred to as the elastic-rebound theory. It is estimated that only 10 percent or less of an earthquake's total energy is radiated as seismic energy. Most of the earthquake's energy is used to power the earthquake fracture growth or is converted into heat generated by friction. Therefore, earthquakes lower the Earth's available elastic potential energy and raise its temperature, though these changes are negligible compared to the conductive and convective flow of heat out from the Earth's deep interior.

Earthquake fault types

There are three main types of fault that may cause an earthquake: normal, reverse (thrust) and strike-slip. Normal and reverse faulting are examples of dip-slip, where the displacement along the fault is in the direction of dip and movement on them involves a vertical component. Normal faults occur mainly in areas where the crust is being extended such as a divergent boundary. Reverse faults occur in areas where the crust is being shortened such as at a convergent boundary. Strike-slip faults are steep structures where the two sides of the fault slip horizontally past each other; transform boundaries are a particular type of strike-slip fault. Many earthquakes are caused by movement on faults that have components of both dip-slip and strike-slip; this is known as oblique slip.

Reverse faults, particularly those along convergent plate boundaries are associated with the most powerful earthquakes, including almost all of those of magnitude 8 or more. Strike-slip faults, particularly continental transforms can produce major earthquakes up to about magnitude 8. Earthquakes associated with normal faults are generally less than magnitude 7.

This is so because the energy released in an earthquake, and thus its magnitude, is proportional to the area of the fault that ruptures and the stress drop. Therefore, the longer the length and the wider the width of the faulted area, the larger the resulting magnitude. The topmost, brittle part of the Earth’s crust, and the cool slabs of the tectonic plates that are descending down into the hot mantel, are the only parts of our planet which can store elastic energy and release it in fault ruptures. Rocks hotter than about 300 degrees Celsius flow in response to stress, they do not rupture in earthquakes. The maximum observed lengths of ruptures and mapped faults, which may break in one go are approximately 1000 km. Examples are the earthquakes in Chile, 1960; Alaska, 1957; Sumatra, 2004, all in subduction zones. The longest earthquake ruptures on strike-slip faults, like the San Andreas Fault (1857, 1906), the North Anatolian Fault in Turkey (1939) and the Denali Fault in Alaska (2002), are about half to one third as long as the lengths along subducting plate margins, and those along normal faults are even shorter.

The most important parameter controlling the maximum earthquake magnitude on a fault is however not the maximum available length, but the available width because the latter varies by a factor of 20. Along converging plate margins, the dip angle of the rupture plane is very shallow, typically about 10 degrees. Thus the width of the plane within the top brittle crust of the Earth can become 50 to 100 km (Tohoku, 2011; Alaska, 1964), making the most powerful earthquakes possible.

Strike-slip faults tend to be oriented near vertically, resulting in an approximate width of 10 km within the brittle crust, thus earthquakes with magnitudes much larger than 8 are not possible. Maximum magnitudes along many normal faults are even more limited because many of them are located along spreading centers, as in Iceland, where the thickness of the brittle layer is only about 6 km.

In addition, there exists a hierarchy of stress level in the three fault types. Thrust faults are generated by the highest, strike slip by intermediate, and normal faults by the lowest stress levels. This can easily be understood by considering the direction of the greatest principal stress, the direction of the force that ‘pushes’ the rock mass during the faulting. In the case of normal faults, the rock mass is pushed down in a vertical direction, thus the pushing force (greatest principal stress) equals the weight of the rock mass itself. In the case of thrusting, the rock mass ‘escapes’ in the direction of the least principal stress, namely upward, lifting the rock mass up, thus the overburden equals the least principal stress. Strike-slip faulting is intermediate between the other two types described above. This difference in stress regime in the three faulting environments can contribute to differences in stress drop during faulting, which contributes to differences in the radiated energy, regardless of fault dimensions.

Earthquakes away from plate boundaries

Where plate boundaries occur within continental lithosphere, deformation is spread out over a much larger area than the plate boundary itself. In the case of the San Andreas fault continental transform, many earthquakes occur away from the plate boundary and are related to strains developed within the broader zone of deformation caused by major irregularities in the fault trace (e.g., the “Big bend” region). The Northridge earthquake was associated with movement on a blind thrust within such a zone. Another example is the strongly oblique convergent plate boundary between the Arabian and Eurasian plates where it runs through the northwestern part of the Zagros mountains. The deformation associated with this plate boundary is partitioned into nearly pure thrust sense movements perpendicular to the boundary over a wide zone to the southwest and nearly pure strike-slip motion along the Main Recent Fault close to the actual plate boundary itself. This is demonstrated by earthquake focal mechanisms.

All tectonic plates have internal stress fields caused by their interactions with neighbouring plates and sedimentary loading or unloading (e.g. deglaciation). These stresses may be sufficient to cause failure along existing fault planes, giving rise to intraplate earthquakes.

Shallow-focus and deep-focus earthquakes

The majority of tectonic earthquakes originate at the ring of fire in depths not exceeding tens of kilometers. Earthquakes occurring at a depth of less than 70 km are classified as 'shallow-focus' earthquakes, while those with a focal-depth between 70 and 300 km are commonly termed 'mid-focus' or 'intermediate-depth' earthquakes. In subduction zones, where older and colder oceanic crust descends beneath another tectonic plate, deep-focus earthquakes may occur at much greater depths (ranging from 300 up to 700 kilometers). These seismically active areas of subduction are known as Wadati-Benioff zones. Deep-focus earthquakes occur at a depth where the subducted lithosphere should no longer be brittle, due to the high temperature and pressure. A possible mechanism for the generation of deep-focus earthquakes is faulting caused by olivine undergoing a phase transition into a spinel structure.

Earthquakes and volcanic activity

Earthquakes often occur in volcanic regions and are caused there, both by tectonic faults and the movement of magma in volcanoes. Such earthquakes can serve as an early warning of volcanic eruptions, as during the Mount St. Helens eruption of 1980. Earthquake swarms can serve as markers for the location of the flowing magma throughout the volcanoes. These swarms can be recorded by seismometers and tiltmeters (a device that measures ground slope) and used as sensors to predict imminent or upcoming eruptions.

Rupture dynamics

A tectonic earthquake begins by an initial rupture at a point on the fault surface, a process known as nucleation. The scale of the nucleation zone is uncertain, with some evidence, such as the rupture dimensions of the smallest earthquakes, suggesting that it is smaller than 100 m while other evidence, such as a slow component revealed by low-frequency spectra of some earthquakes, suggest that it is larger. The possibility that the nucleation involves some sort of preparation process is supported by the observation that about 40% of earthquakes are preceded by foreshocks. Once the rupture has initiated it begins to propagate along the fault surface. The mechanics of this process are poorly understood, partly because it is difficult to recreate the high sliding velocities in a laboratory. Also the effects of strong ground motion make it very difficult to record information close to a nucleation zone.

Rupture propagation is generally modelled using a fracture mechanics approach, likening the rupture to a propagating mixed mode shear crack. The rupture velocity is a function of the fracture energy in the volume around the crack tip, increasing with decreasing fracture energy. The velocity of rupture propagation is orders of magnitude faster than the displacement velocity across the fault. Earthquake ruptures typically propagate at velocities that are in the range 70–90 % of the S-wave velocity and this is independent of earthquake size. A small subset of earthquake ruptures appear to have propagated at speeds greater than the S-wave velocity. These supershear earthquakes have all been observed during large strike-slip events. The unusually wide zone of coseismic damage caused by the 2001 Kunlun earthquake has been attributed to the effects of the sonic boom developed in such earthquakes. Some earthquake ruptures travel at unusually low velocities and are referred to as slow earthquakes. A particularly dangerous form of slow earthquake is the tsunami earthquake, observed where the relatively low felt intensities, caused by the slow propagation speed of some great earthquakes, fail to alert the population of the neighbouring coast, as in the 1896 Meiji-Sanriku earthquake.

Tidal forces

Research work has shown a robust correlation between small tidally induced forces and non-volcanic tremor activity.

Earthquake clusters

Most earthquakes form part of a sequence, related to each other in terms of location and time. Most earthquake clusters consist of small tremors that cause little to no damage, but there is a theory that earthquakes can recur in a regular pattern.

Aftershocks

An aftershock is an earthquake that occurs after a previous earthquake, the mainshock. An aftershock is in the same region of the main shock but always of a smaller magnitude. If an aftershock is larger than the main shock, the aftershock is redesignated as the main shock and the original main shock is redesignated as a foreshock. Aftershocks are formed as the crust around the displaced fault plane adjusts to the effects of the main shock.

Earthquake swarms

Earthquake swarms are sequences of earthquakes striking in a specific area within a short period of time. They are different from earthquakes followed by a series of aftershocks by the fact that no single earthquake in the sequence is obviously the main shock, therefore none have notable higher magnitudes than the other. An example of an earthquake swarm is the 2004 activity at Yellowstone National Park.

Earthquake storms

Sometimes a series of earthquakes occur in a sort of earthquake storm, where the earthquakes strike a fault in clusters, each triggered by the shaking or stress redistribution of the previous earthquakes. Similar to aftershocks but on adjacent segments of fault, these storms occur over the course of years, and with some of the later earthquakes as damaging as the early ones. Such a pattern was observed in the sequence of about a dozen earthquakes that struck the North Anatolian Fault in Turkey in the 20th century and has been inferred for older anomalous clusters of large earthquakes in the Middle East.

Size and frequency of occurrence

It is estimated that around 500,000 earthquakes occur each year, detectable with current instrumentation. About 100,000 of these can be felt. Minor earthquakes occur nearly constantly around the world in places like California and Alaska in the U.S., as well as in Guatemala, Chile, Peru, Indonesia, Iran, Pakistan, the Azores in Portugal, Turkey, New Zealand, Greece, Italy, and Japan, but earthquakes can occur almost anywhere, including New York City, London, and Australia. Larger earthquakes occur less frequently, the relationship being exponential; for example, roughly ten times as many earthquakes larger than magnitude 4 occur in a particular time period than earthquakes larger than magnitude 5. In the (low seismicity) United Kingdom, for example, it has been calculated that the average recurrences are: an earthquake of 3.7–4.6 every year, an earthquake of 4.7–5.5 every 10 years, and an earthquake of 5.6 or larger every 100 years. This is an example of the Gutenberg-Richter law. The number of seismic stations has increased from about 350 in 1931 to many thousands today. As a result, many more earthquakes are reported than in the past, but this is because of the vast improvement in instrumentation, rather than an increase in the number of earthquakes. The United States Geological Survey estimates that, since 1900, there have been an average of 18 major earthquakes (magnitude 7.0–7.9) and one great earthquake (magnitude 8.0 or greater) per year, and that this average has been relatively stable. In recent years, the number of major earthquakes per year has decreased, though this is probably a statistical fluctuation rather than a systematic trend. More detailed statistics on the size and frequency of earthquakes is available from the United States Geological Survey (USGS). Alternatively, some scientists suggest that the recent increase in major earthquakes could be explained by a cyclical pattern of periods of intense tectonic activity, interspersed with longer periods of low-intensity. However, accurate recordings of earthquakes only began in the early 1900s, so it is too early to categorically state that this is the case.

Most of the world's earthquakes (90%, and 81% of the largest) take place in the 40,000 km long, horseshoe-shaped zone called the circum-Pacific seismic belt, known as the Pacific Ring of Fire, which for the most part bounds the Pacific Plate. Massive earthquakes tend to occur along other plate boundaries, too, such as along the Himalayan Mountains.

With the rapid growth of mega-cities such as Mexico City, Tokyo and Tehran, in areas of high seismic risk, some seismologists are warning that a single quake may claim the lives of up to 3 million people.

Induced seismicity

While most earthquakes are caused by movement of the Earth's tectonic plates, human activity can also produce earthquakes. Four main activities contribute to this phenomenon: storing large amounts of water behind a dam (and possibly building an extremely heavy building), drilling and injecting liquid into wells, and by coal mining and oil drilling. Perhaps the best known example is the 2008 Sichuan earthquake in China's Sichuan Province in May; this tremor resulted in 69,227 fatalities and is the 19th deadliest earthquake of all time. The Zipingpu Dam is believed to have fluctuated the pressure of the fault away; this pressure probably increased the power of the earthquake and accelerated the rate of movement for the fault. The greatest earthquake in Australia's history is also claimed to be induced by humanity, through coal mining. The city of Newcastle was built over a large sector of coal mining areas. The earthquake has been reported to be spawned from a fault that reactivated due to the millions of tonnes of rock removed in the mining process.

Measuring and locating earthquakes

Earthquakes can be recorded by seismometers up to great distances, because seismic waves travel through the whole Earth's interior. The absolute magnitude of a quake is conventionally reported by numbers on the Moment magnitude scale (formerly Richter scale, magnitude 7 causing serious damage over large areas), whereas the felt magnitude is reported using the modified Mercalli intensity scale (intensity II–XII).

Every tremor produces different types of seismic waves, which travel through rock with different velocities:

Longitudinal P-waves (shock- or pressure waves)

Transverse S-waves (both body waves)

Surface waves — (Rayleigh and Love waves)

Propagation velocity of the seismic waves ranges from approx. 3 km/s up to 13 km/s, depending on the density and elasticity of the medium. In the Earth's interior the shock- or P waves travel much faster than the S waves (approx. relation 1.7 : 1). The differences in travel time from the epicentre to the observatory are a measure of the distance and can be used to image both sources of quakes and structures within the Earth. Also the depth of the hypocenter can be computed roughly.

In solid rock P-waves travel at about 6 to 7 km per second; the velocity increases within the deep mantle to ~13 km/s. The velocity of S-waves ranges from 2–3 km/s in light sediments and 4–5 km/s in the Earth's crust up to 7 km/s in the deep mantle. As a consequence, the first waves of a distant earth quake arrive at an observatory via the Earth's mantle.

Rule of thumb: On the average, the kilometer distance to the earthquake is the number of seconds between the P and S wave times 8. Slight deviations are caused by inhomogeneities of subsurface structure. By such analyses of seismograms the Earth's core was located in 1913 by Beno Gutenberg.

Earthquakes are not only categorized by their magnitude but also by the place where they occur. The world is divided into 754 Flinn-Engdahl regions (F-E regions), which are based on political and geographical boundaries as well as seismic activity. More active zones are divided into smaller F-E regions whereas less active zones belong to larger F-E regions.

Effects of earthquakes

The effects of earthquakes include, but are not limited to, the following:

Shaking and ground rupture

Shaking and ground rupture are the main effects created by earthquakes, principally resulting in more or less severe damage to buildings and other rigid structures. The severity of the local effects depends on the complex combination of the earthquake magnitude, the distance from the epicenter, and the local geological and geomorphological conditions, which may amplify or reduce wave propagation. The ground-shaking is measured by ground acceleration.

Specific local geological, geomorphological, and geostructural features can induce high levels of shaking on the ground surface even from low-intensity earthquakes. This effect is called site or local amplification. It is principally due to the transfer of the seismic motion from hard deep soils to soft superficial soils and to effects of seismic energy focalization owing to typical geometrical setting of the deposits.

Ground rupture is a visible breaking and displacement of the Earth's surface along the trace of the fault, which may be of the order of several metres in the case of major earthquakes. Ground rupture is a major risk for large engineering structures such as dams, bridges and nuclear power stations and requires careful mapping of existing faults to identify any likely to break the ground surface within the life of the structure.

Landslides and avalanches

Earthquakes, along with severe storms, volcanic activity, coastal wave attack, and wildfires, can produce slope instability leading to landslides, a major geological hazard. Landslide danger may persist while emergency personnel are attempting rescue.

Fires

Earthquakes can cause fires by damaging electrical power or gas lines. In the event of water mains rupturing and a loss of pressure, it may also become difficult to stop the spread of a fire once it has started. For example, more deaths in the 1906 San Francisco earthquake were caused by fire than by the earthquake itself.

Soil liquefaction

Soil liquefaction occurs when, because of the shaking, water-saturated granular material (such as sand) temporarily loses its strength and transforms from a solid to a liquid. Soil liquefaction may cause rigid structures, like buildings and bridges, to tilt or sink into the liquefied deposits. This can be a devastating effect of earthquakes. For example, in the 1964 Alaska earthquake, soil liquefaction caused many buildings to sink into the ground, eventually collapsing upon themselves.

Tsunami

Tsunamis are long-wavelength, long-period sea waves produced by the sudden or abrupt movement of large volumes of water. In the open ocean the distance between wave crests can surpass 100 kilometers (62 miles), and the wave periods can vary from five minutes to one hour. Such tsunamis travel 600-800 kilometers per hour (373–497 miles per hour), depending on water depth. Large waves produced by an earthquake or a submarine landslide can overrun nearby coastal areas in a matter of minutes. Tsunamis can also travel thousands of kilometers across open ocean and wreak destruction on far shores hours after the earthquake that generated them.

Ordinarily, subduction earthquakes under magnitude 7.5 on the Richter scale do not cause tsunamis, although some instances of this have been recorded. Most destructive tsunamis are caused by earthquakes of magnitude 7.5 or more.

Floods

A flood is an overflow of any amount of water that reaches land. Floods occur usually when the volume of water within a body of water, such as a river or lake, exceeds the total capacity of the formation, and as a result some of the water flows or sits outside of the normal perimeter of the body. However, floods may be secondary effects of earthquakes, if dams are damaged. Earthquakes may cause landslips to dam rivers, which collapse and cause floods.

The terrain below the Sarez Lake in Tajikistan is in danger of catastrophic flood if the landslide dam formed by the earthquake, known as the Usoi Dam, were to fail during a future earthquake. Impact projections suggest the flood could affect roughly 5 million people.

Human impacts

An earthquake may cause injury and loss of life, road and bridge damage, general property damage (which may or may not be covered by earthquake insurance), and collapse or destabilization (potentially leading to future collapse) of buildings. The aftermath may bring disease, lack of basic necessities, and higher insurance premiums.

Major earthquakes

One of the most devastating earthquakes in recorded history occurred on 23 January 1556 in the Shaanxi province, China, killing more than 830,000 people (see 1556 Shaanxi earthquake). Most of the population in the area at the time lived in yaodongs, artificial caves in loess cliffs, many of which collapsed during the catastrophe with great loss of life. The 1976 Tangshan earthquake, with death toll estimated to be between 240,000 to 655,000, is believed to be the largest earthquake of the 20th century by death toll.

The largest earthquake that has been measured on a seismograph reached 9.5 magnitude, occurring on 22 May 1960. Its epicenter was near Cañete, Chile. The energy released was approximately twice that of the next most powerful earthquake, the Good Friday Earthquake, which was centered in Prince William Sound, Alaska. The ten largest recorded earthquakes have all been megathrust earthquakes; however, of these ten, only the 2004 Indian Ocean earthquake is simultaneously one of the deadliest earthquakes in history.

Earthquakes that caused the greatest loss of life, while powerful, were deadly because of their proximity to either heavily populated areas or the ocean, where earthquakes often create tsunamis that can devastate communities thousands of kilometers away. Regions most at risk for great loss of life include those where earthquakes are relatively rare but powerful, and poor regions with lax, unenforced, or nonexistent seismic building codes.

Prediction

Many different methods have been developed for predicting the time and place in which earthquakes will occur. Despite considerable research efforts by seismologists, scientifically reproducible predictions cannot yet be made to a specific day or month. However, for well-understood faults the probability that a segment may rupture during the next few decades can be estimated.

Earthquake warning systems have been developed that can provide regional notification of an earthquake in progress, but before the ground surface has begun to move, potentially allowing people within the system's range to seek shelter before the earthquake's impact is felt.

Preparedness

The objective of earthquake engineering is to foresee the impact of earthquakes on buildings and other structures and to design such structures to minimize the risk of damage. Existing structures can be modified by seismic retrofitting to improve their resistance to earthquakes. Earthquake insurance can provide building owners with financial protection against losses resulting from earthquakes.

Emergency management strategies can be employed by a government or organization to mitigate risks and prepare for consequences.

Historical views

From the lifetime of the Greek philosopher Anaxagoras in the 5th century BCE to the 14th century CE, earthquakes were usually attributed to "air (vapors) in the cavities of the Earth." Thales of Miletus, who lived from 625–547 (BCE) was the only documented person who believed that earthquakes were caused by tension between the earth and water. Other theories existed, including the Greek philosopher Anaxamines' (585–526 BCE) beliefs that short incline episodes of dryness and wetness caused seismic activity. The Greek philosopher Democritus (460–371 BCE) blamed water in general for earthquakes. Pliny the Elder called earthquakes "underground thunderstorms."

Earthquakes in culture

Mythology and religion

In Norse mythology, earthquakes were explained as the violent struggling of the god Loki. When Loki, god of mischief and strife, murdered Baldr, god of beauty and light, he was punished by being bound in a cave with a poisonous serpent placed above his head dripping venom. Loki's wife Sigyn stood by him with a bowl to catch the poison, but whenever she had to empty the bowl the poison dripped on Loki's face, forcing him to jerk his head away and thrash against his bonds, which caused the earth to tremble.

In Greek mythology, Poseidon was the cause and god of earthquakes. When he was in a bad mood, he struck the ground with a trident, causing earthquakes and other calamities. He also used earthquakes to punish and inflict fear upon people as revenge.

In Japanese mythology, Namazu (鯰) is a giant catfish who causes earthquakes. Namazu lives in the mud beneath the earth, and is guarded by the god Kashima who restrains the fish with a stone. When Kashima lets his guard fall, Namazu thrashes about, causing violent earthquakes.

Popular culture

In modern popular culture, the portrayal of earthquakes is shaped by the memory of great cities laid waste, such as Kobe in 1995 or San Francisco in 1906. Fictional earthquakes tend to strike suddenly and without warning. For this reason, stories about earthquakes generally begin with the disaster and focus on its immediate aftermath, as in ''Short Walk to Daylight'' (1972), ''The Ragged Edge'' (1968) or ''Aftershock: Earthquake in New York'' (1998). A notable example is Heinrich von Kleist's classic novella, ''The Earthquake in Chile'', which describes the destruction of Santiago in 1647. Haruki Murakami's short fiction collection after the quake depicts the consequences of the Kobe earthquake of 1995.

The most popular single earthquake in fiction is the hypothetical "Big One" expected of California's San Andreas Fault someday, as depicted in the novels ''Richter 10'' (1996) and ''Goodbye California'' (1977) among other works. Jacob M. Appel's widely anthologized short story, ''A Comparative Seismology'', features a con artist who convinces an elderly woman that an apocalyptic earthquake is imminent. In ''Pleasure Boating in Lituya Bay'', one of the stories in Jim Shepard's ''Like You'd Understand, Anyway'', the "Big One" leads to an even more devastating tsunami.

In the film ''2012'' (2009), solar flares (geologically implausibly) affecting the Earth's core caused massive destabilization of the Earth's crust layers. This created destruction planet-wide with earthquakes and tsunamis, foreseen by the Mayan culture and myth surrounding the last year noted in the ''Mesoamerican calendar'' — ''2012''.

Contemporary depictions of earthquakes in film are variable in the manner in which they reflect human psychological reactions to the actual trauma that can be caused to directly afflicted families and their loved ones. Disaster mental health response research emphasizes the need to be aware of the different roles of loss of family and key community members, loss of home and familiar surroundings, loss of essential supplies and services to maintain survival. Particularly for children, the clear availability of caregiving adults who are able to protect, nourish, and clothe them in the aftermath of the earthquake, and to help them make sense of what has befallen them has been shown even more important to their emotional and physical health than the simple giving of provisions. As was observed after other disasters involving destruction and loss of life and their media depictions, such as those of the 2001 World Trade Center Attacks or Hurricane Katrina—and has been recently observed in the 2010 Haiti earthquake, it is also important not to pathologize the reactions to loss and displacement or disruption of governmental administration and services, but rather to validate these reactions, to support constructive problem-solving and reflection as to how one might improve the conditions of those affected.

See also

Seismite

Seismotectonics

Submarine earthquake

Triangle of Life

Marine terrace

References

General references

External links

U.S. Geological Survey Earthquake Hazards Program

Incorporated Research Institutions for Seismology

* IRIS Seismic Monitor - Recent Earthquakes

Open Directory - Earthquakes

Category:Earthquake engineering Category:Geological hazards Category:Seismology

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{{infobox musical artist|name	Tinie Tempah|image_size | background solo_singer| name Tinie Tempah
birth name	Patrick Junior Chukwuemeka Okogwu
nationalism by birth	Nigerian, eastern zone
birth date	November 07, 1988
origin	Plumstead, London,England
genre	Hip Hop, Electro Hop, Grime
occupation	Rapper, songwriter
years active	2005–present
label	Parlophone/DL Records Ltd
Associated acts	Wiz Khalifa, Tinchy Stryder,Snoop Dogg, Chipmunk,Kelly Rowland, Ellie Goulding, JLS, Swedish House Mafia, Wiley, Labrinth, Eric Turner, Travis Barker, DJ Whoo Kid,Bei Maejor
website	}}

Patrick Chukwuemeka Okogwu (born November 7, 1988), better known by his stage name Tinie Tempah, is a British rapper. He made his first mixtape in 2007 with 28 songs, freestyles and remixes, the album features Mz Bratt, Chipmunk and G-Unit. His first album, ''Disc-Overy'', debuted at number one on 10 October 2010 and was preceded by the number-one singles "Pass Out" and "Written in the Stars" and the top-five singles "Frisky" and "Miami 2 Ibiza".

Career History

Early career

In 2006, Tinie gained a great deal of airplay on British music TV channel, Channel AKA, for his song "Tears" and then in late 2007, Tinie Tempah collaborated on a track with grime artist Ultra and producers/songwriters Agent X. The song was titled "Perfect GCD Hood Economics Room 147". He toured with [[Chipmunk (rapper)|Chipmunk ]] in February 2010. His first break as a musician came when Sony launched its PlayStation Portable (PSP) and used a track entitled "Listen To The Vibe" featuring Yasmin and DJ Ironik, and "Atlantic/Warner" for the futuristic racing game, ''Wipeout Pure''. This resulted in a promotional European tour alongside the likes of Sway and Dizzee Rascal.

Tinie and his manager and cousin Dumi Oburota founded the independent label Disturbing London primarily as an official outlet for Tinie's music, but with the idea of also signing other young artists. According to Dumi: "We wanted to have a platform to put out our music and there wasn't any Def Jam or Roc-A-Fella label equivalent in England. [Also] I wanted to create a major independent label with quality artists. I felt like the major labels had lost the passion for music." The activities of the label were initially largely funded by student loans and the proceeds from buying and selling cars.

When scout and music consultant Jade Richardson saw Tinie performing at the 2009 Wireless Festival she called Parlophone Records president Miles Leonard saying: “You’ve got to check out this guy Tinie Tempah. He came on at lunchtime and there’s about 1,000 kids screaming for him. He’s only put out one independent release and he’s got this huge audience.” Leonard and A&R; Nathan Thompson visited Tinie and his manager Dumi at their studio a few weeks later and were hugely impressed to hear about the work they had already done in developing Tinie's career and by the ambitious plans they had for his future. Leonard told HitQuarters: "I thought it was incredible that an artist and manager were doing so much so soon with so little ... That impressed as much as the music."

Tinie announced his signing to Parlophone in October 2009 by running a competition on his blog, with the winner invited to High Tea at Claridges to celebrate the deal.

2010-present: Disc-Overy

Tinie released his debut single "Pass Out" with Parlophone on 28 February 2010, with it entering the UK Singles Chart at number 1. Selling just over 92,000 copies, making this his first number 1 which it remained for two consecutive weeks. Tinie would later perform "Pass Out" on 25 June 2010 at Glastonbury on the Pyramid stage with Snoop Dogg. Tinie then announced his second single, "Frisky", which was released on 6 June 2010 entering the UK Singles Chart at number 2. Tinie supported Rihanna for four dates in May on her 10-date UK tour with Tinchy Stryder and Pixie Lott. Tinie performed at many summer balls at various universities around the United Kingdom. Tinie performed at Radio 1 Big Weekend in Bangor on 22 May 2010 on the In New Music We Trust stage. He also toured with Mr Hudson in May 2010. Tinie Tempah played the Summertime Ball at Wembley Stadium on 6 June 2010, at Wakestock in Abersoch on 3 July 2010, both T4 On The Beach and the Wireless Festival in London's Hyde Park on 4 July, and V Festival on 21 and 22 August 2010. Tinie released his third single "Written in the Stars" on 19 September 2010. This again charted at number 1 in the UK Singles Chart selling over 115,000 copies in its first week, making it his biggest-selling single to date. The song also went on to chart in a number of other countries. Tinie went on to team up with Swedish House Mafia for his fourth single "Miami 2 Ibiza" which was released on 1 October 2010. This went on to reach a peak of number 4 in the UK Singles Chart and his first number 1 in the Netherlands Mega Single Top 100 chart. He released his long-awaited debut album, ''Disc-Overy'' on 4 October 2010 which featured all his previous charted singles. On 11 October 2010, he kicked off his first UK tour which was supported by Chiddy Bang. He went on to win his first 2 MOBO Awards in October. Tinie also featured on the Tinchy Stryder single "Game Over" which was released on 15 November 2010. This reached number 22 on the UK Singles Chart. On 25 December, Tinie released his fifth single "Invincible" featuring Kelly Rowland, which peaked at number 11 on the UK Singles Chart. "Wonderman", featuring Ellie Goulding, was released and was the fifth official single. Tinie joined Usher on the European leg of his OMG Tour in January 2011. Tinie was also nominated for 4 Brit Awards making him the most nominated artist at the awards. His single "Written in the Stars" was used for a WrestleMania XXVII countdown promo during the WWE PPV Royal Rumble on 30 January 2011. It was later confirmed by WWE that it will be the official theme for Wrestlemania XXVII. On 15 February 2011, he won his first ever Brit Award, for Best British Breakthrough Act. He also won a Brit for Best British Single. On 7 March 2011, Tempah expressed his desire for his next album to go triple platinum. "I reckon in 2011, towards the end of it, I'm going to do an arena tour - and sell it out - then I reckon I'm going to release another album, and fingers crossed it can go platinum again, and double platinum, and triple. Let's just sell a million."

In December 2010, Tinie confirmed he is writing a second album, saying there will be a more electronic and live feel to it. It is not yet known what the title will be. Originally intended for a late 2011 release, it is now expected to be released in 2012. During an interview, Tinie commented on his second album: "Yeah I’ve started it already so I’m hoping to get it out by October/November time. I always like to work with different people on each project I do, just so you get a different sound and angle. I will be working with some of the same people I did for the first album, you know what they say ‘if it ain't broke then don’t try and fix it’." According to a recent interview Tinie revealed his hopes of collaborating with some of music's hottest artists saying, "I really want to collaborate with Toronto's very own Drake. I think he's amazing at what he does. I'd also like to collaborate with Adele, Sleigh Bells, Lykke Li, Dev, James Blake ― those are the few that I'd really like to work with." Tinie announced in an interview with ''Rolling Stone'' that his next single is to be called "Till I'm Gone" which will feature Wiz Khalifa and is produced by Stargate. The single and the video song were released at the end of June 2011. Tinie Tempah, world renowned drummer Travis Barker and Irish boxing champion Katie Taylor, joined forces to launch Lucozade’s new ''Yes Campaign'', which signals a repositioning of its sports and energy drink brand. Featuring a performance of Tinie Tempah’s "Simply Unstoppable" with Travis Barker on drums, remixed especially for Lucozade Sport, the campaign was released in Summer 2011.

Awards and nominations

!Year	!Ceremony	!Category	!Nominated work	!Result	!Ref
		Best Newcomer
Best Video
Best UK Act
Best Song
	Hottest Boy
Hottest Hook-up
	The UGG Award (Urban/Garage/Grime)
	Best Newcomer
Best Video
Best Hip-Hop Act
Best Collaboration
	Breakthrough Artist of the Year
Best Male Artist
Best Newcomer
Best Video
Best Song
	Breakthrough Artist
	Best UK and Ireland New Act
		Pop Music	''Disc-Overy''
	Best British Male
Best Breakthrough Act
Best Single
Album of the Year	''Disc-Overy''
	Best Contemporary Song
	Best International Act: UK

Discography

''Disc-Overy'' (2010)

References

External links

Category:English rappers Category:Black British people Category:English people of Igbo descent Category:English people of Nigerian descent Category:Grime artists Category:Black British musicians Category:Igbo musicians Category:People from London Category:British hip hop musicians Category:1988 births Category:Living people

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Name	Busta Rhymes
Religion	Islam
Background	solo_singer
Birth name	Trevor Tahiem Smith, Jr.
Alias
Birth date	May 20, 1972
Origin	Brooklyn, New York, United States
Occupation	Rapper, Actor
Genre	Hip hop
Years active	1989–present
Label	Conglomerate Records
Associated acts	Leaders of the New School, Flipmode Squad, Spliff Star, Def Squad, Wu-Tang Clan, DMX, A Tribe Called Quest, Q-Tip, Mary J.Blige, J Dilla, Missy Elliott, Rampage The Last Boy Scout, Mariah Carey, Dr. Dre, Game, Chris Brown, Lil Wayne
Website	Official Website }}

Trevor Tahiem Smith, Jr., better known by his stage name Busta Rhymes (born May 20, 1972), is an American rapper, producer and actor. Chuck D of Public Enemy gave him the alias Busta Rhymes after NFL wide receiver George "Buster" Rhymes. Early in his career, he was known for his wild style and fashion, and today is best known for his highly skilled rapping technique, which involves rapping at a much faster rate, and to date has received nine Grammy nominations for his musical work.

Early life

Busta was born in Red Hook, Brooklyn, New York, to Jamaican parents Geraldine Green and Trevor Smith in 1972. Smith attended George Westinghouse Information and Technology High School, alongside with Jay-Z, DMX and The Notorious B.I.G. He went to Uniondale High School on Long Island, graduating in 1990.

Music career

Hip-hop crew Leaders of the New School began recording in 1989 and released their debut album ''A Future Without a Past'' in 1991 on Elektra Records. In early 1992 the group appeared on A Tribe Called Quest's posse cut "Scenario," in which Busta's climactic verse propelled him into the cultural consciousness. In 1993, they released ''T.I.M.E. (The Inner Mind's Eye)''. Soon after, however, internal problems arose because of Busta's increasing popularity, and the group broke up on the set of ''Yo! MTV Raps''.

The Coming & When Disaster Strikes (1996-1997)

Busta broke out with a 1996 solo hit single, "Woo Hah!! Got You All in Check" from his platinum record album ''The Coming''. His second album, ''When Disaster Strikes'', released in 1997, produced the hit singles "Put Your Hands Where My Eyes Could See" and "Fire It Up".

Extinction Level Event (Final World Front) (1998-1999)

In 1998, Busta recorded ''Extinction Level Event (Final World Front)''. Its lead single, "Gimme Some More" — which sampled Bernard Herrmann's theme from ''Psycho'' — reached number 6 in the UK singles chart in January 1999. Busta enjoyed further transatlantic success in April when the single "What's It Gonna Be?!", featuring Janet Jackson, reached the US and UK Top 11. The album received prominent notice for featuring the fastest rapping Busta has ever performed, particularly on a song called "Iz They Wildin Wit Us?", featuring a guest appearance by Mystikal.

J/Arista/BMG

Anarchy & Genesis (2000-2001)

After Busta signed to J Records, a label started by the then recently ousted Arista Records chief and founder Clive Davis, he released a greatest hits collection alongside a new album of original work. Continuing the Biblical theme of his previous albums, he titled his record ''Genesis''. The album featured collaborations with Mary J. Blige, P. Diddy, Kelis, and others. Genesis was powered by the hit single with Kelis, "What It Is," and his solo single released in November 2001, "Break Ya Neck." The final single was the summer smash "Pass the Courvoisier, Part II", which featured Pharrell and P. Diddy. Despite the success of the two singles, this album did not sell as well as previous releases.

It Aint Safe No More (2002-2004)

In 2002, Busta released his sixth studio album ''It Ain't Safe No More''. The album was moderately successful, with a hit song featuring Mariah Carey and the Flipmode Squad called "I Know What You Want". Another hit song was "Make It Clap", featuring Spliff Starr. The remix of "Make It Clap" featured Sean Paul. After its release, he left J Records. In 2004, he signed with Dr. Dre's Aftermath Entertainment.

Aftermath/Interscope

The Big Bang (2006)

His seventh studio album, ''The Big Bang'', became the first #1 album of his career. The CD sold over 209,000 copies in its first week to earn the top spot on The Billboard Top 200. The album also became his highest charting album in the UK, peaking at #19. Some of the album was leaked on the Internet, and as a result several songs were left off the album and new ones added. ''The Big Bang'' featured more production by Dr. Dre than Busta's previous releases, as well as appearances by Raekwon and Nas. The singles that have been released from the album are, "Touch It", "I Love My Chick", featuring Kelis and Will.I.Am, "New York Shit",featuring Swizz Beatz and "In The Ghetto". Busta also had a stint opening for Mariah Carey's The Adventures of Mimi Tour. Also, Busta performed with Eminem on "Touch It Remix Part 5" and performed a verse on the aforementioned rapper's song, "I'll Hurt You". On July 17, 2008, Busta left Interscope/Aftermath due to a creative clash with Interscope head Jimmy Iovine.

Universal Motown

Back on My B.S. (2007-2009)

He also made a song featuring Linkin Park called "We Made It". It was later revealed that Busta inked a deal with Universal Motown, who released his eighth studio album, ''Back on My B.S.'', on May 19, 2009. He also appeared on Asher Roth's debut album, ''Asleep in the Bread Aisle''. The album debuted at #5 on the Billboard 200, selling 56,000 copies, and was his first album to not receive an RIAA certification, selling 122,000 copies to date. The singles that have been released from the album are, "Arab Money", featuring Ron Browz, "Hustler's Anthem '09", featuring T-Pain and "Respect My Conglomerate". The song "World Go Round", featuring British singer Estelle, was released in France on April 6, 2009 due to the heavy rotation of a leaked version. The single was released in the UK on July 13, 2009. Due to controversial content, the United Arab Emirates (UAE) has banned the album. ''Back on My B.S.'' was released internationally, but because of one song, "Arab Money", it is not available to buy as a CD there (however, the album can still be purchased via iTunes). According to the National Media Council, the lyrics were considered to be offensive to Arabs and to Islam, and permission for distribution was therefore denied. Some DJs, artists and fans have lambasted the track, saying it portrayed Arabs in a stereotypical way. The first part out of three of the remix by Rhymes contains verses from the Quran. In November, when "Arab Money" was released as a single, DJ Dany Neville and the Iraqi rapper The Narcicyst responded by recorded a reply. Busta later apologized. DJs in the country said they had not received an order banning the record from being spun in nightclubs, and they had mixed feelings on whether the record was offensive or not. DJ Saif of Dubai said: The Emirati DJ Bliss, who has his own show on Radio 1 in Dubai, also says he no longer plays "Arab Money". He added:

Conglomerate Records & E.L.E. 2 (2010-present)

Busta announced that he was working on his ninth studio album, alongside Canadian producer Boi-1da, entitled ''The Chemo''. He says that his next project is 80 percent finished. Busta has reportedly changed the title of his forthcoming Chemo album to Extinction.Level.Event.2 (E.L.E. 2). Some new songs are being considered for the album, including "C'mon (Catch 'Em By Surprise) by Tiësto and Diplo and "Look at Me Now" alongside Chris Brown and Lil Wayne. The trend of album sequels continues with Busta adding another chapter to his 1998 opus E.L.E. (Extinction Level Event): The Final World Front. Busta's manager Chris Lighty sent out the message via Twitter. He said; "Extinction.Level.Event 2 ......prepare yourself." Like the first, E.L.E. 2 is inspired by movies of impending destruction on planet Earth, Lighty said; "From the Intro of the new Busta Album you're going to know you're in trouble and you just turned on 2012 the movie on warp speed,".

DJ Premier, in an August 6, 2010 interview on Conspiracy Worldwide Radio said Busta Rhymes has received over eight beats which he didn't want to use but Premier hoped his next beat would be chosen for inclusion on the album. On DJ Premier's Live From Headqcourterz radio show Premier confirmed that one of his beats were to be included in ''E.L.E. 2''. In 2010, Busta Rhymes formed his new label Conglomerate Records (With later on having rosters such as N.O.R.E., and Spliff Star). He was featured on C'mon (Catch 'Em By Surprise) by Tiësto and Diplo.

Also in, 2011 Rhymes has recorded a song with Chris Brown.

In 2011, Rhymes recorded "Look at Me Now" with Chris Brown and Lil Wayne on Brown's F.A.M.E. album

On May 1, 2011 Rhymes appeared on the launch show for MNET's Big Brother Africa 6: Amplified and performed some of his songs.

In 2011, Busta Rhymes performed at the Gathering of the Juggalos.

Personal life

Religion

Busta Rhymes is Muslim and talked about it in an interview in Hollywood TV.

Busta had been a member of The Nation of Gods and Earths since the age of 15.

Legal issues

On August 20, 2006, he was arraigned for charges of third-degree assault after attacking a man who reportedly spat on his car in New York City on August 12 after the AmsterJam Music Festival on Randall's Island.

On October 24, 2006, he appeared at Manhattan Criminal Court as the district attorney's office attempted to amend previous charges against him to include weapons possession for a machete found in his car. The judge, ShawnDya Simpson, refused to add the charge and adjourned the case.

On February 20, 2007, Busta refused a plea deal offered by the prosecutors office for the assault of his former driver, Edward Hatchett. The deal would have entailed six months in jail and pleading guilty to two assaults, the attack on Hatchett, and the attack on the former fan. The dispute with Hatchett is believed to have originated over back pay Hatchett felt he was owed. Manhattan Criminal Court Judge Becki Rowe offered Busta another option, pleading guilty to third-degree assault. The conditions of the proposed sentence would include five days of community service, two weeks of youth lectures and six months of anger management classes, as well as three years of probation. On March 18, 2008 a judge in New York City sentenced Busta to three years' probation, 10 days' community service, $1250 in fines (plus court costs), and to enroll in a drunken driving program.

On September 25, 2008, he was temporarily refused entry to the United Kingdom due to "unresolved convictions".

On October 14, 2009, a Brooklyn judge ordered Busta to pay a concert goer $75,000 in compensation for an assault which occurred in 2003.

Discography

''The Coming'' (1996)

''When Disaster Strikes'' (1997)

''E.L.E. (Extinction Level Event): The Final World Front'' (1998)

''Anarchy'' (2000)

''Genesis'' (2001)

''It Ain't Safe No More'' (2002)

''The Big Bang'' (2006)

''Back on My B.S.'' (2009)

''TBA '' (2011)

Awards and Nominations

Busta Rhymes has been nominated for 9 Grammy Awards during his 15 year solo career, but has yet to win one.

Grammy Awards

!Year	!Nominated work	!Award	!Result
align=center	"Woo-Hah! Got You All in Check"	Best Rap Solo Performance
align=center	"Put Your Hands Where My Eyes Could See"	Best Rap Solo Performance
align=center	"Dangerous"	Best Rap Solo Performance
align=center	"Gimme Some More"	Best Rap Solo Performance
align=center	"What's It Gonna Be?"	Best Rap Performance By a Duo or Group
align=center	''E.L.E. (Extinction Level Event): The Final World Front''	Best Rap Album
align=center	"Fire"	Best Music Video, Short Form
align=center	"Pass the Courvoisier Pt. 2"	Best Performance By a Duo or Group
align=center	"Touch It"	Best Rap Solo Performance

Busta Rhymes has been nominated for 10 MTV Video Music Awards during his 15 year solo career, but has yet to win one.

MTV Video Music Awards

!Year	!Nominated work	!Award	!Result
align=center	"Woo-Hah! Got You All in Check"	Best Breakthrough Video
align=center	"Put Your Hands Where My Eyes Could See"	Best Rap Video
align=center	"Put Your Hands Where My Eyes Could See"	Best Male Video
align=center	"Put Your Hands Where My Eyes Could See"	Best Breakthrough Video
align=center	"What's It Gonna Be?"	Best Hip-Hop Video
align=center	"Gimme Some More"	Best Breakthrough Video
align=center	"Pass the Courvoisier Pt. 2"	Best Hip-Hop Video
align=center	"I Know What You Want"	Best Hip-Hop Video
align=center	"Touch It"	Best Rap Video
align=center	"Touch It"	Best Male Video

See also

List of number-one U.S. dance hits

List of artists who reached number one on the U.S. Dance chart

References

External links

Category:1972 births Category:Living people Category:Actors from New York City Category:African American film actors Category:African American Muslims Category:African American rappers Category:Aftermath Entertainment artists Category:American people convicted of assault Category:American rappers of Jamaican descent Category:Members of the Nation of Gods and Earths Category:People from Brooklyn Category:Rappers from Long Island Category:Rappers from New York City

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Brett Domino is the alter-ego of Youtube musician Rob J. Madin. As Brett Domino, he is a musician, internet celebrity and TV presenter from Leeds, West Yorkshire, England. He is best known for his YouTube videos, in which he plays mostly covers and medleys of popular songs on the Stylophone and keytar - sometimes with his band, 'The Brett Domino Trio'. The band are notable in that its members (Brett Domino, Steven Peavis and Mitch Hutchinson) all play exclusively keyboard instruments. In a number of recent videos, however, Brett and Steven have diversified to incorporate other instruments, such as ukulele, theremin, recorder, accordion, kalimba and Skoog. Brett and the band have been featured a number of times as part of BBC Radio 1's Chris Moyles Show, and in 2009 the band appeared on ITV's Britain's Got Talent, performing live as the house band on two episodes of ITV2's sister show, Britain's Got More Talent, in the final week.

Brett's Youtube videos have received over 7,000,000 views. A recent video, the Justin Timberlake Medley featuring Trabasacks was posted by Justin Timberlake on his Twitter page and official website.

Brett has also been featured on the websites of Lady Gaga and Ellie Goulding. Another musical alter-ego of Rob J Madin has recently surfaced on YouTube with the name 'Rocco La Bête'. The visual style and editing techniques are very similar to those of the Brett Domino videos.

On November 22, 2010, Brett Domino released a song called "Gillian McKeith", a humorous take on the celebrity during her time in the 10th series of the ITV show I'm a Celebrity... Get Me Out Of Here!. The YouTube video has had over 1,000,000 views. It entered the UK Singles Chart at number 29 on November 28, 2010.

On February 18, 2011, Brett played a specially written song on ''The Chris Moyles Show'' for Chris Moyles' Birthday

On June 10, 2011, Rob J Madin has recently surfaced on Youtube with the name 'C-Bomb', a 'cousin' of Brett Domino's. Here, playing in a style of Dubstep, unlike other Madin videos, 'C-Bomb' is not seen playing any instruments, but does dance, in a similar style to Brett Domino's Lady Gaga - Bad Romance. It also appears that 'C-Bomb' writes his own compositions, as seen with his Youtube video 'Irresistible'

Singles

{|class="wikitable" style=text-align:center; |- !rowspan="2"| Year ! rowspan="2" style="width:200px;"| Single !| Peak chart positions !rowspan="2"| Album |- !style="width:3em;font-size:85%;"|UK |- |rowspan="2"| 2010 |align="left"| "Gillian McKeith" | style="text-align:center;"| 29 | rowspan="2" style="text-align:center;"| ''non-album singles'' |- |align="left"| "Fairytale of New York" (cover, with Alexa Goddard) | style="text-align:center;"| — |}

Albums

Songs Off Youtube

Release date: 1 March 2011

Track listing:

Beat It (2011 Version)

Justin Timberlake Medley

I Feel for You

We Speak No Americano

1980s Stylophone Medley

Bad Romance

Jurassic Park Theme

Ellie Goulding Medley

Hip-Hop Medley

Nelly Furtado Medley

Michael Jackson Medley

Korn / 50 Cent / Tenna Marie Medley

Now 75 Medley

Party In the Park (Radio Aire) Medley

William Tell Overture (Live)

Track By Track Commentary

References

External links

Category:English keyboardists Category:People from Leeds Category:Living people Category:English multi-instrumentalists