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An earthquake is a vibration or abrupt movement of a portion of the Earth's crust. The Earth's crust is slowly moving through plate tectonics. The movements of parts of the Earth's crust can build up stress along fault zones. The large friction on the fracture surfaces prevents a gradual movement in the majority of cases. When the stress becomes too high, a sudden movement occurs along a fault causing an earthquake. Hereby (a part of) the stress is discharged.
Therefore earthquakes in some areas occur with a certain regularity. However, this regularity is not precise enough to allow the precise prediction of earthquakes. Unfortunately, precisely predicting earthquakes is not yet possible, but the areas with elevated seismic risk are known. Due to the discharge of stress at a certain spot, stress is often increased in nearby areas by the displacement during the earthquake. This causes often several aftershocks after a major earthquake.
GSHAP Global Seismic Hazard Map (T. Hengl)
Most earthquakes occur in areas that have a lot of tectonic activity. Mostly along plate boundaries, in subduction or collision zones of tectonic plates, at volcanoes and at active faults. However, there are also earthquakes caused by man, for example by gas extraction. Research has recently indicated that fracking in search of shale gas can cause tremors.
Some known earthquakes from history
- 1556 Shaanxi, China (8 on the Richter scale)
- 1700 Japan, and tsunami in the USA (9 on the Richter scale)
- 1755 Lissabon, Portugal, also tsunami (9 on the Richter scale)
- 1906 San Francisco, USA (7.8 on the Richter scale)
- 1915 Avezzano, Italy (7.0 on the Richter scale)
- 1920 Ningsia province, China (7.8 on the Richter scale)
- 1923 Tokio, Japan (8.3 on the Richter scale)
- 1960 Chili (9.5 on the Richter scale)
- 1964 Prince William Sound, Alaska, USA (9.2 on the Richter scale)
- 1976 Tangshan, China (8.0 on the Richter scale)
- 1985 Michoacán, Mexico (8.1 on the Richter scale)
- 1988 Spitak, Armenia (7.2 on the Richter scale)
- 1995 Kobe, Japan (7.2 on the Richter scale)
- 1999 Istanbul province, Turkey (7.4 on the Richter scale)
- 2003 Bam, Iran (6.6 on the Richter scale)
- 2004 Indian Ocean, tsunami (9.3 on the Richter scale)
- 2010 Port-au-Prince, Haiti (7.0 on the Richter scale)
- 2011 Sendai, Japan (9.0 on the Richter scale)
The place on the surface where the earthquake was most severe in the subsurface is called the epicenter. Further away from the epicenter the strength of the earthquake decreases. The intensity of an earthquake at the epicenter is usually measured and communicated using the Richter scale. This is a logarithmic scale of the amount of energy released by an earthquake. In an earthquake, for example 5 on the Richter scale, 10 times as much energy is released as a tremor of 4 on the Richter scale. Earthquakes from 3 can be felt, from 5 there may be extensive damage, not to mention earthquake measuring 9 on the Richter scale. The amount of damage depends not only on the strength of the quake, but also on the depth of the quake, the condition of the buildings, and the type of sediments at the surface.
Due to excessive vibration of the Earth's crust, buildings may collapse and cracks can occur in the ground. If the quake takes place under the sea, then a tsunami (tidal wave) caused by the sudden movement of the water column can occur. This may cause massive destruction in coastal regions and take many casualties.
The epicenter can be determined with the aid of seismometers. There are two types of earthquake waves in the Earth's crust. The so-called P-wave (primary wave) are longitudinal compression waves that propagate approximately 6 km per second. The S-waves are transverse and travel 3.5 km per second through the Earth's crust. Due to the different speeds of these waves, the distance can be calculated from the seismometer to the epicenter. By combining data from multiple seismometers in various locations, the exact position of the epicenter can be determined.
Strength of earthquakes and their consequences
The lightest earthquakes on the Richter scale are very common and the most severe earthquakes only occur once every few years.
- Less than 2.0 are common but are not felt by people
- 2.0 - 3.5 Are barely felt by people
- 3.5 - 5.0 Will usually felt but little damage
- 5.0 - 6.0 Moderate earthquake with mild to severe damage to structures, depending on the condition
- 6.0 - 7.0 Heavy earthquake, major damage to buildings
- 7.0 - 8.0 Very Heavy devastating earthquake
- greater than 8.0 Extremely powerful earthquake, serious destruction in large areas
Do you have additional information for this article? Please contact the Fossiel.net Team.