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Earthquake

result of a sudden release of energy in the Earth's crust that creates seismic waves
(Redirected from Earthquakes)
Damage from the San Francisco, California earthquake in 1906

An earthquake (or quakes, tremors) is the shaking of the surface of the Earth. They are caused by sudden movements of the Earth's tectonic plates. Earthquakes can be extremely violent or so slight that they only register on instruments.

The study of earthquakes is called seismology.[1] Earthquakes are usually quite brief, but may repeat. The sudden release of tension in the tectonic plates sends waves of energy that travel through the Earth. Seismology studies the cause, frequency, type and size of earthquakes.

There are large earthquakes and small earthquakes. Large earthquakes can take down buildings and cause death and injury. Earthquakes are measured using observations from seismometers. The magnitude of an earthquake, and the intensity of shaking, is usually reported on the Richter scale. The Richter Scale was invented by Charles Francis Richter in 1935. On the scale, 2 is scarcely noticeable, and magnitude 5 (or more) causes damage over a wide area.

An earthquake under the ocean can cause a tsunami. This can cause just as much death and destruction as the earthquake itself. Landslides can happen, too. Earthquakes are part of the Earth's rock cycle. The impact can be measured by a seismometer. It detects the vibrations caused by an earthquake. It puts these movement on a seismograph. The strength, or magnitude, of an earthquake is measured using the Richter scale. The Richter scale is numbered 0-9.

Scientists cannot view a major earthquake beforehand. They do know where earthquakes may occur, such as close to the fault lines. 

Advice on what to do in an earthquake:

a) If you are indoor:-

  • Take cover under a table or bench. If there is no table or desk, sit against a wall away from things that might fall on you and stay away from windows, bookcases or tall, heavy furniture.
  • Wait in your safety spot until the shaking stops and then check to see if you are hurt. Check others around you too. Move carefully and look out for fallen things.
  • There may be aftershocks or smaller earthquakes quite soon after. So be prepared.
  • If you want to leave the building after the shaking stops , use the stairs, never use elevators

b) If you are outdoor :-

  • Stay away from tall buildings, trees, street lamps, and power lines. Crouch down and cover your head.

Contents

HistoryEdit

Earthquakes sometimes hit cities and kill hundreds of thousands of people. Most earthquakes happen along the Pacific Ring of Fire but the biggest ones mostly happen in other places. Tectonically active places are places where earthquakes or volcanic eruptions are frequent.

Causes of an earthquakeEdit

Earthquakes are caused by tectonic movements in the Earth's crust. The main cause is when tectonic plates ride one over the other, causing orogeny (mountain building), and severe earthquakes.

The boundaries between moving plates form the largest fault surfaces on Earth. When they stick, motion between the plates leads to increasing stress. This continues until the stress rises and breaks, suddenly allowing sliding over the locked portion of the fault. This releases the stored energy as shock waves. The San Andreas fault in San Francisco, and Rift valley in Africa are faults like this.

Earthquake fault typesEdit

 
Replica of ancient seismometer with pendulum sensitive to ground tremors. In Luoyang in 133 AD, it detected an earthquake 400 to 500 km (250 to 310 mi) away

There are three main types of geological fault that may cause an earthquake: normal, reverse (thrust) and strike-slip. Normal faults occur mainly in areas where the crust is being extended. Reverse faults occur in areas where the crust is being shortened. Strike-slip faults are steep structures where the two sides of the fault slip horizontally past each other.

Earthquake clustersEdit

Most earthquakes form part of a sequence, related to each other in terms of location and time.[2] Most earthquake clusters consist of small tremors which cause little to no damage, but there is a theory that earthquakes can recur in a regular pattern.[3]

A foreshock is an earthquake that occurs before a larger earthquake, called the mainshock.

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. Aftershocks are formed as the crust adjusts to the effects of the main shock.[2]

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 notably higher magnitudes than the other. An example of an earthquake swarm is the 2004 activity at Yellowstone National Park.[4]

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 occurred in the North Anatolian fault in Turkey in the 20th century.[5][6]

TsunamiEdit

Animation of the 2011 Sendai tsunami.

Tsunami or a chain of fast moving waves in the ocean caused by powerful earthquakes is a very serious challenge for people's safety and for earthquake engineering. Those waves can inundate coastal areas, destroy houses and even swipe away whole towns.[7] This is a danger for the whole mankind.

Unfortunately, tsunamis can not be prevented. However, there are warning systems[8] which may warn the population before the big waves reach the land to let them enough time to rush to safety.

Earthquake-proofingEdit

Some places, such as Japan or California, have many earthquakes and many inhabitants. There, it is good practice to construct houses and other buildings which will resist collapse in an earthquake. This is called seismic design or "earthquake-proofing".

 
The Haitian National Palace after at the 2010 Haiti earthquake.

Earthquake-proof buildings are constructed to withstand the destructive force of an earthquake. This depends upon its type of construction, shape, mass distribution, and rigidity. Different combinations are used. Square, rectangular, and shell-shaped buildings can withstand earthquakes better than skyscrapers. To reduce stress, a building's ground floor can be supported by extremely rigid, hollow columns, while the rest of the building is supported by flexible columns inside the hollow columns. Another method is to use rollers or rubber pads to separate the base columns from the ground, allowing the columns to shake parallel to each other during an earthquake.

To help prevent a roof from collapsing, builders make the roof out of light-weight materials. Outdoor walls are made with stronger and more reinforced materials such as steel or reinforced concrete. During an earthquake flexible windows may help hold the windows together so they don’t break.

SourcesEdit

  1. Earth Science. Austin, Texas 78746-6487: Holt, Rinehart Winston. 2001. ISBN 0-03-055667-8. 
  2. 2.0 2.1 "What are aftershocks, foreshocks, and earthquake clusters?". 
  3. "Repeating earthquakes". United States Geological Survey. January 29, 2009. Retrieved May 11, 2009. 
  4. "Earthquake swarms at Yellowstone". USGS. Retrieved 2008-09-15. 
  5. Amos Nur (2000). "Poseidon’s horses: plate tectonics and earthquake storms in the late [Bronze Age Aegean and Eastern Mediterranean"]. Journal of Archaeological Science 27: 43–63. doi:10.1006/jasc.1999.0431. ISSN 0305-4403. http://water.stanford.edu/nur/EndBronzeage.pdf. 
  6. "Earthquake storms". Horizon (BBCtv series). 9pm 1 April 2003. Retrieved 2007-05-02.  Check date values in: |date= (help)
  7. USGS Poster of the Near the East Coast of Honshu, Japan Earthquake of 11 March 2011 - Magnitude 8.9
  8. Pacific Tsunamy Warning Center

Other websitesEdit