Earthquake: Difference between revisions
imported>Nereo Preto m (some links) |
mNo edit summary |
||
| (8 intermediate revisions by 6 users not shown) | |||
| Line 1: | Line 1: | ||
{{subpages}} | |||
{{dambigbox|Earthquake|Earth}} | |||
{{TOC|right}} | |||
An '''earthquake''' is a shaking of the ground, normally caused by movements on a geologic [[fault (geology|fault]]. Earthquakes range in size from those barely perceptible by sensitive instruments to "great earthquakes" such as the one which struck Indonesia in 2004. | An '''earthquake''' is a shaking of the ground, normally caused by movements on a geologic [[fault (geology|fault]]. Earthquakes range in size from those barely perceptible by sensitive instruments to "great earthquakes" such as the one which struck Indonesia in 2004. | ||
According to the theory of [[plate tectonics]], pieces of the earth's [[crust]], called plates, are constantly moving relative to each other. Since the crust is brittle, | According to the theory of [[plate tectonics]], pieces of the earth's [[crust]], called plates, are constantly moving relative to each other. Since the crust is brittle, accommodating these movements causes breaks in the crust, called '''faults'''. Movement along faults is rarely smooth, and often, faults will remain "locked" for a period of time due to frictional resistance. When the driving force overcomes the [[friction]], the material on each side of the fault will suddenly move relative to the other side. This movement causes shaking which is felt most strongly close to the fault and dissipates with distance. | ||
The shaking | The shaking caused by an earthquake can be strong enough to knock down people, animals, and buildings, and can trigger [[landslide]]s. | ||
Earthquakes are very frequent, though the frequency varies inversely with the size of the earthquake - earthquakes as large as the Indonesia Earthquake of 2004 occur once or twice a century worldwide, while earthquakes barely perceptible by humans occur several times a day throughout the world. | Earthquakes are very frequent, though the frequency varies inversely with the size of the earthquake - earthquakes as large as the Indonesia Earthquake of 2004 occur once or twice a century worldwide, while earthquakes barely perceptible by humans occur several times a day throughout the world. | ||
==Earthquake terms== | ==Earthquake terms== | ||
;'''hypocenter''' - the location in the earth where the earthquake movement began. | ;'''[[hypocenter]]''' - also known as the focus, it is the location in the earth where the earthquake movement began. | ||
;'''epicenter''' - the location on the surface of the earth directly above the hypocenter. | ;'''[[epicenter]]''' - the location on the surface of the earth directly above the hypocenter. | ||
;'''[[seismic waves]]''' - waves of energy expelled from the hypocenter in a circular fashion. | |||
;'''[[seismology]]''' - the study of earthquakes. The prefix seismo- also starts words such as seismograph (an instrument for measuring earthquake strength), and seismologist (one who studies earthquakes). | |||
==Types of earthquakes== | ==Types of earthquakes== | ||
There are three main types of earthquake: | |||
*'''Tectonic''' earthquakes are the most common and are caused by pressure build-up in between plates. | |||
*'''Volcanic''' earthquakes occur in conjunction with volcanic eruptions. | |||
*'''Collapse''' earthquakes occur when mines cave in. | |||
*'''Explosion''' earthquakes are caused by explosion of nuclear devices or other strong explosives.<ref>[http://scign.jpl.nasa.gov/learn/eq2.htm Southern California Education]</ref> | |||
==Earthquake waves== | ==Earthquake waves== | ||
The kinds of waves are as follows: | |||
*P (primary) waves, the fastest wave | |||
*S (secondary) waves, the most dangerous type of wave | |||
*Surface waves, either Love waves or Raleigh waves.<ref>[http://scign.jpl.nasa.gov/learn/eq6.htm Southern California Education]</ref> | |||
==Measurement of earthquakes== | ==Measurement of earthquakes== | ||
Earthquakes are measured by geologists and seismologists in two main ways, '''magnitude''' and '''intensity'''. The magnitude of an earthquake is a property of the earthquake as a whole, and measures the energy released during the earthquake. The intensity of an earthquake is a property of both the earthquake and a specific location, and measures the shaking felt at any given location. An earthquake with a specific magnitude will have a range of intensities, dropping with distance from the hypocenter. | Earthquakes are measured by geologists and seismologists in two main ways, '''magnitude''' and '''intensity'''. The magnitude of an earthquake is a property of the earthquake as a whole, and measures the energy released during the earthquake. The intensity of an earthquake is a property of both the earthquake and a specific location, and measures the shaking felt at any given location. An earthquake with a specific magnitude will have a range of intensities, dropping with distance from the hypocenter. | ||
| Line 21: | Line 33: | ||
Intensity is measured by the [[Modified Mercalli scale]], the [[Japan Meteorological Agency seismic intensity scale]], or peak ground [[acceleration]]. The three scales (and some historic ones) can be roughly calibrated to each other. After an earthquake, based on reports or instrument readings, a map showing the variation of intensity across the area where the earthquake was felt can be produced. Maps predicting the maximum intensity expected at given locations are prepared for planning purposes. | Intensity is measured by the [[Modified Mercalli scale]], the [[Japan Meteorological Agency seismic intensity scale]], or peak ground [[acceleration]]. The three scales (and some historic ones) can be roughly calibrated to each other. After an earthquake, based on reports or instrument readings, a map showing the variation of intensity across the area where the earthquake was felt can be produced. Maps predicting the maximum intensity expected at given locations are prepared for planning purposes. | ||
==Preparing for earthquakes== | |||
Preparing for earthquakes can be done in such ways as: | |||
*creating emergency kits, | |||
*building earthquake-proof structures, | |||
*knowing to do things such as hide under tables to protect oneself. | |||
==References== | |||
<references />[[Category:Suggestion Bot Tag]] | |||
Latest revision as of 16:00, 9 August 2024
An earthquake is a shaking of the ground, normally caused by movements on a geologic fault. Earthquakes range in size from those barely perceptible by sensitive instruments to "great earthquakes" such as the one which struck Indonesia in 2004.
According to the theory of plate tectonics, pieces of the earth's crust, called plates, are constantly moving relative to each other. Since the crust is brittle, accommodating these movements causes breaks in the crust, called faults. Movement along faults is rarely smooth, and often, faults will remain "locked" for a period of time due to frictional resistance. When the driving force overcomes the friction, the material on each side of the fault will suddenly move relative to the other side. This movement causes shaking which is felt most strongly close to the fault and dissipates with distance.
The shaking caused by an earthquake can be strong enough to knock down people, animals, and buildings, and can trigger landslides.
Earthquakes are very frequent, though the frequency varies inversely with the size of the earthquake - earthquakes as large as the Indonesia Earthquake of 2004 occur once or twice a century worldwide, while earthquakes barely perceptible by humans occur several times a day throughout the world.
Earthquake terms
- hypocenter - also known as the focus, it is the location in the earth where the earthquake movement began.
- epicenter - the location on the surface of the earth directly above the hypocenter.
- seismic waves - waves of energy expelled from the hypocenter in a circular fashion.
- seismology - the study of earthquakes. The prefix seismo- also starts words such as seismograph (an instrument for measuring earthquake strength), and seismologist (one who studies earthquakes).
Types of earthquakes
There are three main types of earthquake:
- Tectonic earthquakes are the most common and are caused by pressure build-up in between plates.
- Volcanic earthquakes occur in conjunction with volcanic eruptions.
- Collapse earthquakes occur when mines cave in.
- Explosion earthquakes are caused by explosion of nuclear devices or other strong explosives.[1]
Earthquake waves
The kinds of waves are as follows:
- P (primary) waves, the fastest wave
- S (secondary) waves, the most dangerous type of wave
- Surface waves, either Love waves or Raleigh waves.[2]
Measurement of earthquakes
Earthquakes are measured by geologists and seismologists in two main ways, magnitude and intensity. The magnitude of an earthquake is a property of the earthquake as a whole, and measures the energy released during the earthquake. The intensity of an earthquake is a property of both the earthquake and a specific location, and measures the shaking felt at any given location. An earthquake with a specific magnitude will have a range of intensities, dropping with distance from the hypocenter.
Magnitude was originally measured by the Richter magnitude scale, which is a logarithmic scale based on the movements an earthquake caused on a Wood-Anderson seismograph at a distance of 100km. The Richter magnitude scale, often called the "Richter scale", was developed by Charles Richter for use in California, and does not produce accurate results for the largest earthquakes. Several other scales have been proposed to supplement or modify the Richter scale, the most generally used one now being the moment magnitude scale, which is also a logarithmic scale, based on the seismic moment of an earthquake; the moment magnitude scale has been calibrated to yield comparable numbers to the Richter scale.
Intensity is measured by the Modified Mercalli scale, the Japan Meteorological Agency seismic intensity scale, or peak ground acceleration. The three scales (and some historic ones) can be roughly calibrated to each other. After an earthquake, based on reports or instrument readings, a map showing the variation of intensity across the area where the earthquake was felt can be produced. Maps predicting the maximum intensity expected at given locations are prepared for planning purposes.
Preparing for earthquakes
Preparing for earthquakes can be done in such ways as:
- creating emergency kits,
- building earthquake-proof structures,
- knowing to do things such as hide under tables to protect oneself.