Quake (natural phenomenon)
A quake is the result when the surface of a planet, moon or star begins to shake, usually as the consequence of a sudden release of energy transmitted as seismic waves, and potentially with great violence.[1]
Types of quakes include:
Contents
Earthquake
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An earthquake is a phenomenon that results from the sudden release of stored energy in the Earth's crust that creates seismic waves. At the Earth's surface, earthquakes may manifest themselves by a shaking or displacement of the ground and sometimes cause tsunamis, which may lead to loss of life and destruction of property. An earthquake is caused by tectonic plates (sections of the Earth's crust) getting stuck and putting a strain on the ground. The strain becomes so great that rocks give way and fault lines occur.
Moonquake
A moonquake is the lunar equivalent of an earthquake (i.e., a quake on the Moon). They were first discovered by the Apollo astronauts. Moonquakes are much weaker than the largest earthquakes, though they can last for up to an hour, due to the lack of water to dampen seismic vibrations.[2]
Information about moonquakes comes from seismometers placed on the Moon by Apollo astronauts from 1969 through 1972. The instruments placed by the Apollo 12, 14, 15 and 16 functioned perfectly until they were switched off in 1977.
According to NASA, there are at least four different kinds of moonquakes:
- Deep moonquakes (~700 km below the surface, probably tidal in origin)
- Meteorite impact vibrations
- Thermal moonquakes (the frigid lunar crust expands when sunlight returns after the two-week lunar night)
- Shallow moonquakes (20 or 30 kilometers below the surface)
The first three kinds of moonquakes mentioned above tend to be mild; however, shallow moonquakes can register up to 5.5 on the Richter scale. Between 1972 and 1977, 28 shallow moonquakes were observed. On Earth, quakes of magnitude 4.5 and above can cause damage to buildings and other rigid structures.
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Marsquake
A marsquake is a quake that occurs on the planet Mars. A recent study suggests that marsquakes occur every million years. This suggestion is related to recently found evidence of Mars's tectonic boundaries.[3]
Venusquake
A venusquake is a quake that occurs on the planet Venus.
A venusquake may have caused a new scarp and a landslide to form. An image of the landslides was taken in November 1990 during the first flight around Venus by the Magellan spacecraft. Another image was taken on July 23, 1991 as the Magellan spacecraft revolved around Venus for the second time. Each image was 24 kilometers (14.4 miles) across and 38 kilometers (23 miles) long, and was centered at 2° south latitude and 74° east longitude. The pair of Magellan images shows a region in Aphrodite Terra, within a steeply sloping valley that is cut by many fractures (faults).
Planetquake
Lua error in package.lua at line 80: module 'strict' not found. Planetquake is the generic term for quakes occurring on terrestrial planets, since current observational technology cannot penetrate to the solid core of gaseous planets.
Sunquake
A sunquake is a quake that occurs on the Sun.
Seismic waves produced by sunquakes occur in the photosphere and can travel at velocities of 22,000 miles per hour for distances up to 250,000 miles before fading away.[4]
On July 9, 1996, a sunquake was produced by an X2.6 class solar flare and its corresponding coronal mass ejection. According to researchers who reported the event in Nature, this sunquake was comparable to an earthquake of a magnitude 11.3 on the Richter scale. That represents a release of energy approximately 40,000 times greater than that of the devastating 1906 San Francisco earthquake, and far greater than that of any earthquake ever recorded. It is unclear how such a relatively modest flare could have liberated sufficient energy to generate such powerful seismic waves.[4][5]
The ESA and NASA spacecraft SOHO records sunquakes as part of its mission to study the sun.
Starquake
A starquake is an astrophysical phenomenon that occurs when the crust of a neutron star undergoes a sudden adjustment, analogous to an earthquake on Earth. A paper published in 2003 in Scientific American by Kouveliotou, Duncan & Thompson[6] suggests these starquakes to be the source of the giant gamma ray flares that are produced approximately once per decade from soft gamma repeaters. Starquakes are thought to result from two different mechanisms. One is the huge stresses exerted on the surface of the neutron star produced by twists in the ultra-strong interior magnetic fields. A second cause is a result of spindown. As the neutron star loses angular velocity due to frame-dragging and by the bleeding off of energy due to it being a rotating magnetic dipole, the crust develops an enormous amount of stress. Once that exceeds a certain amount, the shape adjusts itself to a shape closer to non-rotating equilibrium: a perfect sphere. The actual change is believed to be on the order of micrometers or less, and occurs in less than a millionth of a second.
The largest recorded starquake was detected on December 27, 2004 from the ultracompact stellar corpse (magnetar) SGR 1806-20, which created a quake equivalent to a 22 on the Richter Scale. The quake, which occurred 50,000 light years from Earth, released gamma rays equivalent to 1037 kW in intensity. Had it occurred within a distance of 10 light years from Earth, the quake would have possibly triggered a mass extinction.[7]
See also
References
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