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Who made the song earthquake?
ForeverMount EverestStill Don't Know My NameGeniusAll For UsFormulaLabrinth/Songs
When was Earthquake song released?
2011Earthquake / Released
Is Labrinth a producer?
Timothy Lee McKenzie (born 4 January 1989), better known by his stage name Labrinth, is a British musician, singer, songwriter, rapper and record producer. Initially he began professionally as a producer, but Simon Cowell signed him to his record label Syco Music as a solo act.
What album is Earthquake on?
"Earthquake" is a song by British musician Labrinth which features long-time collaborator Tinie Tempah. The track was released on 23 October 2011 in the United Kingdom as the second single from the artist's debut studio album, Electronic Earth (2012).
What is Maxwell's biggest song?
Best Maxwell Songs of All Time – Top 10 TracksAscension (Don't Ever Wonder) - Remastered 2021.Pretty Wings - uncut.Fortunate.This Woman's Work - Remastered 2021.Sumthin' Sumthin' - Remastered 2021.Fire We Make. Alicia Keys, Maxwell.Lifetime - Remastered 2021.Get to Know Ya - Remastered 2021.More items...
What was EMS first song?
More from The Source's controversial leak in an effort to present Em as the 'Rap's Hitler,' Foolish Pride is Eminem's oldest song known to this day. Dated way back to 1988 when he was only 16, young Marshall had just broken up with a black girlfriend and took on his songs to make racist remarks.
Who wrote Elliot's song in Euphoria?
It was written by Labrinth, his girlfriend Muzhda "Muz" Zemar-McKenzie, and Zendaya. The song was included in a longer version in the season two finale of Euphoria. At the 74th Primetime Emmy Awards, the song was nominated for Outstanding Original Music and Lyrics.
Did Labrinth create Euphoria?
In April 2022, Euphoria Season 2 Official Score (From the HBO Original Series) composed by Labrinth, was released. It earned him an additional two Primetime Emmy Award nominations for the songs "I'm Tired" and "Elliot's Song", written alongside Zendaya.
What do producers in music do?
What is a Music Producer? A music producer, or record producer, assists an artist with their recording project, bringing their vision to fruition and guiding their sound along the way.
Is Earthquake based on a true story?
Review: 1988 Armenian tragedy plays out in 'Earthquake' The script by Hrant Barsegyan, Arsen Danielyan, Aleksey Gravitskiy and Sergey Yudakov reportedly reflects true stories of rescue and survival culled from documentation and the accounts of eyewitnesses.
Did Earfquake go platinum?
Its official remix by Channel Tres was released on October 4, 2019. "Earfquake" is Tyler, the Creator's highest charting song in the US, peaking at number 13 on the Billboard Hot 100....Certifications.RegionCertificationCertified units/salesUnited Kingdom (BPI)Gold400,000United States (RIAA)4× Platinum4,000,0005 more rows
Why is farruko album called 167?
More Stories by Jessica. After three years of working on his album and creating music “for the love of it, not for the trends,” Farruko presents his new studio album La 167 via Sony Music Latin, named after one of the main highways in Puerto Rico, near his hometown.
What was Omarions biggest hit?
Let Me Hold You. Bow Wow Featuring Omarion. 05.28.05. ... Ice Box. Omarion. 12.16.06. ... O. Omarion. 01.22.05. ... Girlfriend. Bow Wow & Omarion. 11.17.07. 12.29.07.I Get It In. Omarion Featuring Gucci Mane. 11.14.09. 12.19.09.Entourage. Omarion. 08.26.06. 09.02.06.Touch. Omarion. 06.25.05. 07.30.05. ... Screwin. Summer Walker & Omarion. 11.20.21. 11.20.21.More items...
What was Feargal Sharkey biggest hit?
A Good HeartHis best-known solo material is the 1985 UK chart-topping single penned by Lone Justice frontwoman Maria McKee, "A Good Heart", which went to No. 1 in several countries including the UK in late 1985. He also had a UK Top 5 hit in 1986 with "You Little Thief".
What was Sisqo first song?
Sisqó's solo debut, Unleash the Dragon, was released on Def Soul Records in November 1999. Unleash the Dragon sold moderately at first, until the February 2000 release of its second single, the novelty "Thong Song".
What was Sigrid's biggest hit?
The song peaked at number six on the Norwegian Singles Chart....Track listing.No.TitleLength1."Strangers"3:53
Why is an earthquake dangerous?
Over the centuries, earthquakes have been responsible for millions of deaths and an incalculable amount of damage to property. Depending on their i...
What are earthquake waves?
Earthquake waves, more commonly known as seismic waves, are vibrations generated by an earthquake and propagated within Earth or along its surface....
How is earthquake magnitude measured?
Magnitude is a measure of the amplitude (height) of the seismic waves an earthquake’s source produces as recorded by seismographs. Seismologist Cha...
Where do earthquakes occur?
Earthquakes can occur anywhere, but they occur mainly along fault lines (planar or curved fractures in the rocks of Earth’s crust), where compressi...
How does a tectonic earthquake occur?
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, which leads to a form of stick-slip behavior. 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.
How do earthquakes manifest themselves?
At the Earth's surface, earthquakes manifest themselves by shaking and displacing or disrupting 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.
What type of fault is responsible for earthquakes?
Reverse faults, particularly those along convergent plate boundaries, are associated with the most powerful earthquakes, megathrust earthquakes, including almost all of those of magnitude 8 or more. Megathrust earthquakes are responsible for about 90% of the total seismic moment released worldwide. 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. For every unit increase in magnitude, there is a roughly thirtyfold increase in the energy released. For instance, an earthquake of magnitude 6.0 releases approximately 32 times more energy than a 5.0 magnitude earthquake and a 7.0 magnitude earthquake releases 1,000 times more energy than a 5.0 magnitude of earthquake. An 8.6 magnitude earthquake releases the same amount of energy as 10,000 atomic bombs like those used in World War II.
How does an earthquake start?
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 (330 ft) 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.
What is the name of the wave that causes the Earth to shake?
An earthquake (also known as a quake, tremor or temblor) is the shaking of the surface of the Earth resulting from a sudden release of energy in the Earth 's lithosphere that creates seismic waves.
How much more energy does a 6.0 earthquake release?
For instance, an earthquake of magnitude 6.0 releases approximately 32 times more energy than a 5.0 magnitude earthquake and a 7.0 magnitude earthquake releases 1,000 times more energy than a 5.0 magnitude of earthquake.
What is the velocity of rupture?
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, which is independent of earthquake size.
What is the purpose of the USGS in natural hazards?
The mission of the USGS in natural hazards is to develop and apply hazard science to help protect the safety, security, and economic well-being of the Nation.
How deep is the San Andreas fault?
The San Andreas Fault is more than 650 miles long and extends to depths of at least 10 miles. Many other smaller faults like the Hayward (Northern California) and the San Jacinto (Southern California) branch from and join the San Andreas Fault Zone. The Pacific Plate grinds northwestward past the North American Plate at a rate ...
How much does the Pacific Plate grind?
The Pacific Plate grinds northwestward past the North American Plate at a rate of about two inches per year. Parts of the San Andreas Fault system adapt to this movement by constant "creep" resulting in many tiny shocks and a few moderate earth tremors.
How can the risks of an earthquake be reduced?
The risks that earthquakes pose to society, including death, injury, and economic loss, can be greatly reduced by (1) better planning, construction, and mitigation practices before earthquakes happen, and (2)... The severity of an earthquake can be expressed in terms of both intensity and magnitude. However, the two terms are quite different, and ...
Why do earthquakes happen?
An earthquake is caused by a sudden slip on a fault. The tectonic plates are always slowly moving, but they get stuck at their edges due to friction. When the stress on the edge overcomes the friction, there is an earthquake that releases energy in waves that travel through the earth's crust and cause the shaking that we feel.
How many people died in the 2004 tsunami?
Geological Survey (USGS), 2004 was the deadliest year for earthquakes since the Renaissance Age, making it the second most fatal in recorded history, with more than 275,950 deaths reported from the magnitude 9.0 earthquake and subsequent tsunami that hit the Indian Ocean on Dec. 26.
What is the mission of the USGS?
The mission of the USGS in natural hazards is to develop and apply hazard science to help protect the safety, security, and economic well-being of the Nation. The costs and consequences of natural hazards can be enormous, and each year more people and infrastructure are at risk.
How often do earthquakes occur?
Very great earthquakes occur on average about once per year. Over the centuries they have been responsible for millions of deaths and an incalculable amount of damage to property. San Francisco earthquake of 1906. Crowds watching the fires set off by the earthquake in San Francisco in 1906, photo by Arnold Genthe.
How many types of waves are there?
There are four principal types of elastic waves: two, primary and secondary waves, travel within Earth, whereas the other two, Rayleigh and Love waves, called surface waves, travel along its surface. In addition, seismic waves can be produced artificially by explosions.
What causes earthquakes?
Earthquake, any sudden shaking of the ground caused by the passage of seismic waves through Earth ’s rocks. Seismic waves are produced when some form of energy stored in Earth’s crust is suddenly released, usually when masses of rock straining against one another suddenly fracture and “slip.”. Earthquakes occur most often along geologic faults, ...
Where does the energy released by earthquakes come from?
It is estimated that 80 percent of the energy presently released in earthquakes comes from those whose epicentres are in this belt . The seismic activity is by no means uniform throughout the belt, and there are a number of branches at various points.
How is energy released?
The energy can be released by elastic strain, gravity, chemical reactions, or even the motion of massive bodies. Of all these the release of elastic strain is the most important cause, because this form of energy is the only kind that can be stored in sufficient quantity in the Earth to produce major disturbances.
Where is seismic activity located?
There also are striking connected belts of seismic activity, mainly along oceanic ridges —including those in the Arctic Ocean, the Atlantic Ocean, and the western Indian Ocean —and along the rift valleys of East Africa. This global seismicity distribution is best understood in terms of its plate tectonic setting.
When did the 5.5 earthquake occur?
earthquake epicentres. Global seismic centres for earthquakes of magnitude 5.5 and greater occurring between 1975 and 1999. Encyclopædia Britannica, Inc. About 50,000 earthquakes large enough to be noticed without the aid of instruments occur annually over the entire Earth.
What is an earthquake?
An earthquake is what happens when two blocks of the earth suddenly slip past one another. The surface where they slip is called the fault or fault plane. The location below the earth’s surface where the earthquake starts is called the hypocenter, and the location directly above it on the surface of the earth is called the epicenter.
Why does the earth shake when there is an earthquake?
The energy radiates outward from the fault in all directions in the form of seismic waves like ripples on a pond. The seismic waves shake the earth as they move through it, and when the waves reach the earth’s surface, they shake the ground and anything on it, like our houses and us!
How do scientists measure the size of earthquakes?
The size of an earthquake depends on the size of the fault and the amount of slip on the fault, but that’s not something scientists can simply measure with a measuring tape since faults are many kilometers deep beneath the earth’s surface. So how do they measure an earthquake? They use the seismogram recordings made on the seismographs at the surface of the earth to determine how large the earthquake was (figure 5). A short wiggly line that doesn’t wiggle very much means a small earthquake, and a long wiggly line that wiggles a lot means a large earthquake. The length of the wiggle depends on the size of the fault, and the size of the wiggle depends on the amount of slip.
Is there such a thing as earthquake weather? Can some animals or people tell when an earthquake is about to hit?
If weather does affect earthquake occurrence, or if some animals or people can tell when an earthquake is coming, we do not yet understand how it works.
How is the intensity of an earthquake determined in the Philippines?
In the Philippines, the intensity of an earthquake is determined using the PHIVOLCS Earthquake Intensity Scale (PEIS). There are two types of earthquakes: tectonic and volcanic earthquakes. Tectonic earthquakes are produced by sudden movement along faults and plate boundaries.
How many seismic monitoring stations are there in the Philippines?
At present, PHIVOLCS operates 108 (as of December 2020) seismic monitoring stations all over the Philippines. These stations are equipped with seismometers that detect and record earthquakes. Data is sent to the PHIVOLCS Data Receiving Center (DRC) to determine earthquake parameters such as magnitude, depth of focus and epicenter. Together with reported felt intensities in the area (if any), earthquake information is released once these data are determined.
What is the name of the point where an earthquake starts?
The earthquakes originate in tectonic plate boundary. The focus is point inside the earth where the earthquake started, sometimes called the hypocenter, and the point on the surface of the earth directly above ...
What is the intensity of an earthquake?
Intensity on the other hand, is the strength of an earthquake as perceived and felt by people in a certain locality. It is a numerical rating based on the relative effects to people, objects, environment, and structures in the surrounding. The intensity is generally higher near the epicenter. It is represented by Roman Numerals (e.g. II, IV, IX).
How to measure the strength of an earthquake?
There are two ways by which we can measure the strength of an earthquake: magnitude and intensity. Magnitude is proportional to the energy released by an earthquake at the focus. It is calculated from earthquakes recorded by an instrument called seismograph.
Where earthquakes happen
The lithosphere is the outermost layer of the Earth. It consists of the crust and uppermost mantle. The lithosphere is broken into extremely large slabs called tectonic plates. These plates move around on the molten layer beneath.
What causes earthquakes
We already know that earthquakes occur mostly, but not always, at the boundaries of tectonic plates. Let’s look at the mechanisms behind this.
Intraplate earthquakes
Less than 10 percent of all earthquakes occur far from plate boundaries. These are called intraplate earthquakes. These happen when pressure builds up and the earth’s crust is stretched or squeezed until it rips.
Faults and boundaries
The deadliest earthquake ever recorded occurred in 1556 and struck Shaanxi province, China. It killed an estimated 830,000 people. Afterward, buildings were made from softer materials like bamboo and wood rather than stone.
Recording and locating earthquakes
Seismologists cannot predict earthquakes but once a quake has happened, they can pinpoint its starting point, or epicenter, with accuracy.
Measuring earthquake intensity
Seismologists used to assign magnitudes to earthquakes using the Richter scale.
When did the remix of "Earfquake" come out?
Its official remix by Channel Tres was released on October 4, 2019. "Earfquake" is Tyler, the Creator's highest charting song in the US, peaking at number 13 on the Billboard Hot 100. It was also ranked 14th on Billboard ' s 100 Best Songs of 2019 list.
Who wrote the song "Earfquake"?
Tyler initially wrote the song for Canadian singer Justin Bieber, who turned down the song. Tyler then asked Barbadian singer Rihanna to provide vocals to the hook believing the song would be big, but she also rejected the song. Tyler instead kept in his own raw vocals. "Earfquake" was initially leaked online on May 7, 2019.
Overview
Effects of earthquakes
The effects of earthquakes include, but are not limited to, the following:
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 …
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, which leads to a form of stick-slip behavior. Once the fault has locked, continued relative motion between the plat…
Intensity and magnitude of earthquakes
Shaking of the earth is a common phenomenon that has been experienced by humans from the earliest of times. Before the development of strong-motion accelerometers, the intensity of a seismic event was estimated based on the observed effects. Magnitude and intensity are not directly related and calculated using different methods. The magnitude of an earthquake is a single value that describes the size of the earthquake at its source. Intensity is the measure of s…
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 El Salvador, Mexico, Guatemala, Chile, Peru, Indonesia, the Philippines, Iran, Pakistan, the Azores in Portugal, Turkey, New Zealand, Greece, Italy, India, Nepal and Japan. Larger earthquakes occur less freq…
Induced seismicity
While most earthquakes are caused by movement of the Earth's tectonic plates, human activity can also produce earthquakes. Activities both above ground and below may change the stresses and strains on the crust, including building reservoirs, extracting resources such as coal or oil, and injecting fluids underground for waste disposal or fracking. Most of these earthquakes have small magnitudes. The 5.7 magnitude 2011 Oklahoma earthquake is thought to have been caused by di…
Measuring and locating earthquakes
The instrumental scales used to describe the size of an earthquake began with the Richter magnitude scale in the 1930s. It is a relatively simple measurement of an event's amplitude, and its use has become minimal in the 21st century. Seismic waves travel through the Earth's interior and can be recorded by seismometers at great distances. The surface wave magnitude was developed in the 1950s as a means to measure remote earthquakes and to improve the accuracy for large…
Major earthquakes
One of the most devastating earthquakes in recorded history was the 1556 Shaanxi earthquake, which occurred on 23 January 1556 in Shaanxi, China. More than 830,000 people died. Most houses in the area were yaodongs—dwellings carved out of loess hillsides—and many victims were killed when these structures collapsed. The 1976 Tangshan earthquake, which killed between 240,000 and 655,000 people, was the deadliest of the 20th century.