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Seismic Monitoring
SEISMIC MONITORING IN WESTERN AUSTRALIA- the University of Western Australia network
- the Regional Seismic Network
- temporary Pilbara deployment
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INTRODUCTIONBefore the days of modern instrumentation, only earthquakes which were felt by humans entered the historical record. Nowdays earthquakes are detected by sensitive seismographs, which are installed by research bodies in places of interest around the globe. These can detect minute ground motions, from earthquakes thousands of kilometres distant. Most governments, and many universities run their own networks of seismographs. Most West Australian seismographs are operated by the federal government body, Geoscience Australia, which operates out of Canberra, ACT, and maintains an Australia-wide network. For a brief history on the development of seismographs, click here. Most of the world's earthquakes occur along the boundaries of the Earth's tectonic plates. Earthquakes within the plates (intraplate earthquakes) are far less common, but still can be large and devastating. Earthquakes are not uncommon in Australia, although many Australian earthquakes pass unnoticed by the general population (because they are relatively small, or may have occurred in a relatively remote part of the country). The two principal bodies responsible for monitoring earthquakes in Australia are Geoscience Australia in Canberra, ACT, and the Seismology Research Centre in Melbourne, Vic. About 400 earthquakes a year are detected by instruments (seismographs) in a region between Geraldton and Albany, WA, called the Southwest Seismic Zone (SWSZ). This region is possibly the most seismically active part of the Australian continent. If you feel an earthquake, you are encouraged to report it by filling in this on-line form. The map below shows the locations of seismographs in Western Australia 
Seismographs in the region of Perth 
< /> THE GEOSCIENCE AUSTRALIA SEISMOGRAPH NETWORKThe table below shows seismographs operated in Western Australia by Geoscience Australia. As the locations may be moved over time, and subtle changes are made to the station code, the original station codes are given. For a more up-to-date list, contact Geoscience Australia, Canberra ACT. Note that there are other stations in Western Australia operated by other agencies, and these are described elsewhere in this section. LOCATION | CODE | LONG | LAT | AGENCY | REMARKS | | MUNDARING | MUN | 116.2083 | -31.9783 | GA | opened 1959 | | KALGOORLIE | KLG | 121.458 | -30.7837 | GA | replaced by Kambalda | | KUNUNURRA | KNA | 128.7667 | -15.75 | GA | | | MARBLE BAR | MBL | 119.8333 | -21.16 | GA | replaced by MBWA | | MORAWA | MRWA | 116.0388 | -29.0683 | GA | | | FITZROY XING | FITZ | 125.639 | -18.102 | GA | replaced FITX | | KELLERBERRIN | KLBN | 117.7546 | -31.5915 | GA | replaced KLB | | BALLIDU | BLDU | 116.7091 | -30.6147 | GA | replaced BAL | | NARROGIN | NWAO | 117.2339 | -32.9269 | GA/USGS | | | ROCKY GULLY | RKGY | 116.9773 | -34.6094 | GA | replaced RKG | | GIRALIA | GIRL | 114.243 | -22.643 | GA | corrected coords | | FORREST | FORT | 128.059 | -30.779 | GA | replaced FORR | | MEEKATHARRA | MEEK | 118.6145 | -26.6378 | GA | opened June 1992 | | KAMBALDA | KMBL | 121.8821 | -31.3669 | ga | replaced KLGA and COOL |
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| In addition to these instruments, Geoscience Australia operates a number of "strong motion recorders" or accelerographs, at a number of sites around the state. These are normally triggered by large events, and do not provide data for all seismic events. |
UWA seismograph networkA Sprengnether long - period seismograph is operated in the School of Earth and Geographical Sciences. Images from this recorder are regularly posted to http://cyllene.uwa.edu.au/~vdent/SEISMIC During its period of operation, quite a number of large events have produced good seismograms, and can be found by following the link to ARCHIVES/EQgallery on the above site. In addition, a number of seismograms from the BRSA station at Mt. Nebo, near Brisbane ( operated by the University of Queensalnd) are included in the directory. Some of the events to be found in ARCHIVES/EQgallery ( see file EQ-index.txt in that directory) are tabulated below. | FILE NAME | DATE | EVENT | MAGN | GMT | | 19 Sep 2006 | Sth of Java | 6.1 | 1358 | | UWA.271.gif | 28 Sep 2006 | Samoa | 6.9 | 0622 | | UWA.290.gif | 17 Oct 2006 | New Britain, PNG | 6.5 | 0125 | | UWA.295.gif | 22 Oct 2006 | Southeast Indian Ridge | 6.1 | 0855 | | geology.245.gif | 02 Sep 2007 | Bougainville, PNG | 6.8 | 1018 | | QLD.208.gif | 27 Jul 2007 | New Hebrides | 6.3 | 1446 | | QLD.213.gif | 01 Aug 2007 | Vanuatu | 6.9 | 1708 | | QLD.220.gif | 08 Aug 2007 | Java, Sunda Arc | 7.6 | 1704 | | QLD.245.gif | 01 Sep 2007 | Bougainville, PNG | 6.8 | 1018 | | QLD.354.gif | 21 Dec 2007 | Nth Island, New Zealand | 6.7 | 0755 | | QLD.356.gif | 23 Dec 2007 | West Irian | 6.4 | 0711 | | | | | |
In addition to the long period seismograph at UWA, the university runs PSN (public seismic network) stations at a number of locations, including Broome and York High Schools in Western Australia, and Gundaroo Primary School in New South Wales. There is potential to set up seismographs at other locations at a nominal cost. Interested schools or other parties should indicate this on the site feed-back form found elsewhere on this web site. |
The Regional Seismic NetThe "Regional Seismic Network" is the name given to a network of low-cost seismographs being developed by the Australian Centre for Geomechanics, based on the UWA campus in Perth, WA. It started operation in 2006 with the establishment of a number of stations at mine sites in the Kalgoorlie - Kambalda region of Western Australia. It then expanded to include networks in the Agnew - Leinster nickel - mining region of Western Australia, and the Beaconsfield Gold Mine in Tasmania For more information on this network, click here, or to view recent data, follow this link
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Joint UWA/ ANU/GA Pilbara seismic deploymentA temporary network of Reftec seismographs was deployed in the Pilbara region of WA in late 2006. The aim of the project is to help identify neotectonic processes in the region. It is a joint project between the UWA, the Austalian National University and Geoscience Australia. It is also supported financially by Woodside Petroleum and Chevron Oil. For more inforation on this project, contact Dr. Myra Keep of the University of Western Australia
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MORE ON SEISMIC RECORDINGMost often, seismographs have a single sensor, sensing vibrations in the vertical plane. These are called one - component stations. The better equipped stations have three components, mounted in the vertical plane, and also NS and EW. All seismic stations these days have an accurate clock with which the incoming signals are timed. Today, these clocks are normally GPS controlled. Geoscience Australia stations today have a telecommunication link, which sends the data directly to GA in Canberra ACT. Waveforms for user-selectable periods are available on-line, by visiting a website operated by GA www.ga.gov.au/urban/waveform.jsp Below - GA technician Owen McConnel, who maintains the GA seismic network in Western Australia, from a base in Weshpool, Perth. 
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