Swiss Seismological Service
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| Agency overview | |
|---|---|
| Headquarters | Zurich, Switzerland |
| Employees | ca. 60 |
| Agency executive |
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| Website | http://www.seismo.ethz.ch/ |
The Swiss Seismological Service (Template:Lang-de, Template:Lang-fr, Template:Lang-it, Template:Lang-rm) at ETH Zurich is the federal agency responsible for monitoring earthquakes in Switzerland and its neighboring countries and for assessing Switzerland’s seismic hazard. When an earthquake happens, the SED informs the public, authorities, and the media about the earthquake’s location, magnitude, and possible consequences.
History
The beginnings of the SED trace back to the establishment of the Erdbebenkommission in 1878. In 1914, the earthquake monitoring mandate was defined in a federal law. Thus, what had been a voluntary activity previously was transformed into an institution. In its present form as a nondepartmental unit of ETH Zurich, the SED has been in existence since 2009. [1]
Earthquake monitoring
More than 100 seismic monitoring stations installed and serviced by the SED constantly monitor earthquake activity in Switzerland and its neighboring countries. These stations can be classified into three types:
- Broadband network: Highly sensitive broadband seismometers register even the slightest ground tremors caused by weak local as well as strong global earthquakes. The stations are preferably installed in remote locations on solid rock.
- Strong motion network: Seismometers that are suited for measuring strong local tremors. These are mainly located in settlement areas and high-risk regions.
- Temporary networks: Seismometers with which the SED densifies the network in order to monitor increased natural seismic activity, or any other seismic activity in the context of construction or industry projects by third-party assignment.[2]
Earthquake hazard in Switzerland
In comparison with other European countries Switzerland faces a medium seismic hazard, but there are regional differences: In Valais, Basel, the St. Gallen Rhine Valley, Mittelbünden, the Engadine, and Central Switzerland more earthquakes are registered than in other regions. However, earthquakes may occur anytime and anywhere in Switzerland.
A strong earthquake with a magnitude of approximately 6 occurs every 50 to 100 years on average. The last time an earthquake of such magnitude was recorded was in 1946 near Sierre in Valais.
The strongest earthquake in Switzerland so far had a magnitude of approximately 6.6 and destroyed large parts of the city of Basel in 1356. If such an earthquake were to occur in Basel today, several thousand fatalities, tens of thousands of seriously and slightly injured people, and property damage on the order of approximately CHF 140 billion could be expected.
The best protection measures against the effects of an earthquake are an earthquake-resistant building design and securing objects that may topple. 90 percent of the buildings in Switzerland are not built to a seismic code, and it is not clear to what extent they could withstand a strong earthquake. Only few cantons have
statutory regulations requiring adherence to construction standards for earthquake-resistant building.
[3][4]
Alert in Case of an Earthquake
Earthquakes can neither be predicted nor prevented. However, the SED records the ground tremors around the clock. Within approximately 90 seconds details about the time, location, magnitude, and possible effects of an earthquake are displayed on the website www.seismo.ethz.ch.
The SED automatically reports any noticeable earthquakes to the authorities and the media. At the same time, this information is transmitted to the SED’s 24-hour on-call service via pager, e-mail, and SMS. This service is also available to the authorities and the media for further information about current earthquakes, and prepares background information that is published on the website.
In case of earthquakes that cause major damage worldwide, the SED additionally informs the Swiss Humanitarian Aid Unit (SHA).
[5]
Research and Teaching
Besides earthquake monitoring and the assessment of seismic hazard, the researchers of the SED are involved in numerous national and international research projects, which are largely financed by third parties. This guarantees the permanent exchange of information across national borders. Fields in which the SED researchers are involved include, for example, glacial and engineering seismology, static seismology, induced seismic activity, as well as the monitoring of landslides and seismotectonics. The training of junior researchers also plays an important role for the SED. This is done with lectures and seminars that are integral parts of the teaching program at ETH, as well as through the supervision of master’s and doctoral theses.[6]
Nuclear-test-ban treaty monitoring
In 1996, the UN countries decided to draft an agreement on the ban of nuclear tests. An international monitoring system was established to control the adherence to this agreement. The SED contributes by supplying the authority in charge in Vienna with data recorded by the seismic station in the Davos region, which was constructed for exactly this purpose. For example, the seismic station already recorded the corresponding ground shaking twelve minutes after the nuclear test in North Korea in 2013. [7]
External links
References
- ^ "History Swiss Seismological Service". www.seismo.ethz.ch. Retrieved 2014-02-04.
- ^ "Earthquake Monitoring Switzerland". www.seismo.ethz.ch. Retrieved 2014-02-04.
- ^ "Earthquake hazard and risk". www.seismo.ethz.ch. Retrieved 2014-02-04.
- ^ "Scenario Earthquake Basel". www.seismo.ethz.ch. Retrieved 2014-02-04.
- ^ "Warning". www.seismo.ethz.ch. Retrieved 2014-02-04.
- ^ "Research and Teaching". www.seismo.ethz.ch. Retrieved 2014-02-04.
- ^ "Nuclear-test-ban treaty monitoring". www.seismo.ethz.ch. Retrieved 2014-02-04.