The Eskdalemuir Observatory is a UK national environmental observatory located near Eskdalemuir, Dumfries and Galloway, Scotland. Along with Lerwick and Hartland, Eskdalemuir is one of three permanent geomagnetic observatories in the United Kingdom.
Built in 1904, its remote location was chosen to minimise electrical interference with geomagnetic instruments, which were relocated here from Kew Observatory in London in 1908 after the spread of electric tramcars led to excessive electromagnetic interference there. [1]
The observatory is situated in the valley of the White Esk river at an altitude of 242m, and so represents the climate of highland in northern Great Britain.
It currently monitors:
The observatory is managed by the British Geological Survey and the UK Met Office.
The area has a low background of seismic activity, so is ideal for these measurements.
Shortly after 19:00 GMT on 21 December 1988, the observatory's seismometers recorded the ground impact of Pan Am Flight 103, which crashed into the nearby town of Lockerbie 23 kilometres (14 mi) away after being destroyed by a bomb. The event registered 1.6 on the Richter magnitude scale. [2]
There is a second seismic array approximately 3 km north of the main observatory established by the United Kingdom Atomic Energy Authority, which has been managed by Güralp Systems Ltd since 2002 on behalf of AWE Blacknest which provides the UK part of the international monitoring network of the Comprehensive Test Ban Treaty. This network allows covert nuclear tests to be detected via their seismic signatures. At Eskdalemuir it consists of an array covering 10 square km, consisting of two intersecting lines of 10 pits containing seismometers, a seismological vault and a recording laboratory. [3]
Following the conventions of Kew Observatory, which preceded Eskdalemuir as a national geophysical laboratory, atmospheric electricity measurements formed a key part of the early operations. Atmospheric ion measurements [4] were made by Lewis Fry Richardson. [5] As Eskdalemuir is a relatively clean site distant from major towns and cities, the atmospheric electricity measurements have been analysed for global signals which are typically obscured at urban sites. [6] The measuring technology followed that of Kew in employing a Kelvin water dropper electrometer for potential gradient measurements, [7] changing to a radioactive polonium probe during the 1930s. The Eskdalemuir potential gradient was found to be correlated with measurements made simultaneously on the Carnegie research ship. [6]
Seismology is the scientific study of earthquakes and the generation and propagation of elastic waves through the Earth or other planetary bodies. It also includes studies of earthquake environmental effects such as tsunamis as well as diverse seismic sources such as volcanic, tectonic, glacial, fluvial, oceanic microseism, atmospheric, and artificial processes such as explosions and human activities. A related field that uses geology to infer information regarding past earthquakes is paleoseismology. A recording of Earth motion as a function of time, created by a seismograph is called a seismogram. A seismologist is a scientist works in basic or applied seismology.
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The following outline is provided as an overview of and topical guide to geophysics:
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Harry Oscar Wood (1879–1958) was an American seismologist who made several significant contributions in the field of seismology in the early twentieth-century. Following the 1906 earthquake in San Francisco, California, Wood expanded his background of geology and mineralogy and his career took a change of direction into the field of seismology. In the 1920s he co-developed the torsion seismometer, a device tuned to detect short-period seismic waves that are associated with local earthquakes. In 1931 Wood, along with another seismologist, redeveloped and updated the Mercalli intensity scale, a seismic intensity scale that is still in use as a primary means of rating an earthquake's effects.
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