The most common means of displaying seismic monitoring data is called a seismogram. Traditionally these were drawn by ink on paper, but today are usually created by computers using digital data. GeoNet seismograms of National Network sites can be seen here.
You read a seismogram like you are reading these words; the earliest time is at the top left and then goes along the line to the end and then starts at the left of the next line. The top-left is therefore the oldest data and the bottom-right the most recent. All the seismograms shown in these pages cover a 24-hour period.
The seismograms shown on the GeoNet website do not display 'real-time' data. The volume of data required to be sent across the internet to show the ground as it moves is too great to display all the seismograms in 'real-time'. Instead, each seismogram is produced every 5 minutes and the web page updated as each new image becomes available. If you want to keep track of changes over a period of time remember to hit the 'refresh' icon on your browser every so often.
GeoNet seismographs typically record the ground movement 100 times a second. To download a seismogram at this resolution from a web page would take a long time, even using fast broadband. To reduce the download time we draw a seismogram that displays only one data point each second. You can see the main features of a seismogram, but not all of the detail. GeoNet scientists use these seismograms for a 'quick look' at what is happening and make other kinds of seismograms if they want to look in more detail.
The label on the top-left of the seismogram in Fig. 1 (i.e. OTVZ/10-EHZ/CH) says exactly which seismograph's data are shown (see the FAQ). On the top-right is the time of the most recent data (i.e. 2007/08/25 17:40:00 NZST). On the right side is the plotting scale (i.e. Scale: 200) and along the left and bottom are the time axes.
No. Some sites are noisier than others and tend to be plotted at a scale that shows a smaller signal (these sites have a larger scale number). To plot these sites at the same scale as nearby, quieter sites would result in a seismogram completely blue (or red) and would show no useful information.
An earthquake typically shows as a signal that is much larger than that of the normal background.
A nearby earthquake usually has a very sudden onset and decays away relatively quickly - usually less than 5 minutes (see Fig. 2). With a more distant earthquake you may be able to see both the P- and S-waves (see Fig. 3) and the earthquake decays away more slowly. Because of the limited resolution of the seismograms you cannot always see both the P- and S-waves, especially for nearby earthquakes.
A seismogram is coloured red if is clipped, i.e. the largest parts of the signal are not shown. If this was not done then a large earthquake would obscure much of the seismogram from view. So if the signal is red, the real size is larger than is shown on the seismogram.
In the central North Island volcanic region (Ruapehu to the Bay of Plenty coast) earthquakes frequently occur as swarms.
A swarm is a sequences of many earthquakes, usually in a short time period (hours to days), without a single clear largest event. Swarms are often seen on seismograms from monitoring sites at or near the volcanoes.
The seismogram in Fig. 4 is from Handcock Road (a site between Taupō and Rotorua) shows a typical earthquake swarm, starting at about the 12 hour mark and continuing until the end of the plot. The larger of the earthquakes would be locatable, and some of those probably felt nearby.
The main noise sources on seismograms are wind and vehicle traffic.
The main noise sources on seismograms are wind and vehicle traffic, and this makes volcano monitoring difficult.
In Fig. 5 wind noise is noticeable between about 13 and 8 hours previously, then there is a short calmer period before a stronger wind starts (around 7 hours previously) and continues until the end of the seismogram.
In some cases individual vehicles can be seen and in other cases there are so many vehicles that the ground vibrates continuously and looks like wind:
Other sites sometimes show noise that is particular to that site. Examples include seismographs on Mount Ruapehu that record noise produced by skifield chair lifts (see Fig. 8).
These images are used to appraise the frequency of local earthquakes and the level of ground tremor at a volcano.
The production of these images is computationally intensive so there is no guarantee that the images are available for every site, nor that the style of the images will stay the same. A typical set of images for a volcano monitoring site are:
The above URLs point to the latest images for the seismometer at site HBAZ. As long as we need to produce images for this site and there is a seismometer at the location then the URLs are valid. For more information about each seismic site, including opening and any closing dates, see our DELTA database. You may also wish to view the seismic network maps or read about how we interpret these images.