MS Word version of this file Before you do this you will need a copy of the program "WinQuake" running on your system. You can get a copy of the program from a link on the Quake Trackers website (www.quaketrackers.org.nz) on the Locate your own earthquake page. Downloading seismograms: On the Quake Trackers home page, select NZ schools seismogram database page. On the database page click on Retrieve seismograms from database and now you are ready to select which seismograms you wish to view. You can choose an earthquake by entering its date (year, month,day). Alternatively, you can select a particular seismograph station. In the example shown, the 12 May 1999 earthquake is selected, and we
want seismograms from Sacred Heart College, St. Marys College, Wainuiomata College,
Kuranui College, and Victoria University. We didnt select any particular
orientation, so all 3 will be retrieved. |
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We only want the earthquake just after 10:00 so we have unselected the earthquake at 08:52 by clicking the include boxes for that earthquake. Now click the Package Files button. This puts the files (seismograms) all together into one
zipped file so you only need to download once, instead of downloading each
seismogram individually. |
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The final step before we can start WinQuake and look at the seismograms
is to unzip the download.zip file. |
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After Winzip starts up, just click on Extract and follow the
instructions. Once again when it asks you where to put the files, you can put the files
anywhere you wish but one suggestion is the WinQuake\data folder (directory) so that the
files will be available to you as soon as you start WinQuake. |
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| Using WINQUAKE
To start Winquake Click on the Shortcut to the Winquake
icon if you have it Once Winquake has started, click on the line that lists the time, school and seismograph component you wish to look at. OR if your seismograms are in another folder than the
Winquake\data folder (directory) then click on "Change
directory... so you can select the directory with the seismograms that you wish
to view. |
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| Move the cursor down or up to select the line you wish (or hold the Shift key down to select a few) then click on Open File. In the example above the seismogram recorded on the N-S seismometer at
Kuranui College on 12 May 99 at 10:09 am has been selected. |
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| Part three: Analysing a seismogram. Now we can determine the P wave and S wave arrival times by moving the P & S markers to the appropriate times. Winquake calculates the time difference and uses this to calculate the distance to the epicentre. To show the P & S markers press CTRL R or click on
PS button. |
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If other seismometers recorded the earthquake we can use the distance calculated from several P-S time differences to locate the epicentre of the earthquake. The Epicentre is the place on the surface of the earth that is directly above the earthquake centre or Hypocenter. After picking the P and S arrival times at several stations that
recorded this earthquake, click on the Locate event button earthquake, click
on the Locate event button |
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One additional step was needed to get the circles to overlap at the same point, which was to guess the depth of the earthquake and then set the depth by clicking on the Tables menu. In the Tables box, set the depth to 33 km (a good first guess) and select IASP91 as the Current Table. If you also click on Save as Default, 33 km will always be your starting guess. In New Zealand, earthquakes can be as deep as 350 km or as shallow as 5 km. Magnitude If the seismometers multiplying factor is already included with the seismogram data, an initial estimate of the magnitude will be shown as soon as the P and S waves are picked. The magnitude can be determined manually by selecting Magnitude Marker (Ml and Ms) from the Calculate menu. Then click and drag the M marker to the largest amplitude of the seismogram. If there is an Ml?? after Mag:, on the line above the seismogram, click on the Calculate menu and choose Magnitude Settings. In the Ml and Ms correction factor box, enter 0.001. This number relates to how much each seismograph amplifies the ground motion. Depending on the station and the earthquake, this number might need to vary anywhere between 0.0003 and 0.003 to get a match with magnitudes estimated by GNS. Once this number has been added then proceed as above.
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