by Duygu kiyan & giuseppe Maggio, DIAS
Exploring the Earth beneath County Antrim
with the GEMINI Passive Seismic Array
24 April 2025
Having joined
the GEMINI project at Dublin Institute for Advanced Studies (DIAS) in October
2024, Giuseppe Maggio immediately started scouting and permitting for seismic
station installation in Co. Antrim, Northern Ireland.
In January, Giuseppe,
along with Colin Hogg (Senior Technician at DIAS) and members of the Geological
Survey of Northern Ireland, then began installing the passive seismic stations.
These stations will record data for the next 18 months to capture naturally
occurring ground vibrations — from distant ocean tides to local human
activities such as traffic and industrial operations; from natural events like
storms to minor and distant earthquakes. The seismic vibrations move at
different speeds through rock layers of different density and temperature and
reach the passive seismic stations at different times. The wave data can then
be processed by scientists to image the subsurface.
The data
collected from seismic stations across County Antrim will be analysed to give
us a better understanding of the layers of rock beneath our feet — all the way
down to 5 km below the Earth’s surface.
Did you know?
A
teleseismic earthquake is a tremor caused by an earthquake that originates more
than 1,000 km away from the recording station.
How do we collect the data? Keeping our
sensors safe from water is crucial, so the team came up with a clever way to
protect the electronics. Here is how it works: First, we dig a hole about 50–80
cm deep and 30 cm wide. We pour some concrete in the bottom to give it a solid
base. Then, we place a plastic drum down into the concrete and fill the bottom
of the drum with cement to make a nice, flat floor for the seismic sensor to
sit on. Once the cement has dried, we carefully place the sensor inside, making
sure it is perfectly level and pointing North — this helps us figure out which
direction the seismic waves are coming from. After that, we hook up all the
cables and seal everything up safely inside the drum. The cables run out to a
connection box, which links the sensor to its power source — a solar panel (1.2
m by 0.8 m) and battery (12 Volt) setup — so it can keep working out in the
field without a problem.
So far we have
deployed 22 stations, 4 stations to go!
What does the
data look like? The plots in the image show seismic data recorded by our station ANT21
during Storm Éowyn. The first plot displays how ground motion changed over
time, revealing the storm’s seismic signature. The second plot, called a
spectrogram, shows the frequencies of these signals — helping us see how the
storm’s energy was distributed over time at different frequencies, as captured
by ANT21. We can also see other signals created by nearby traffic, which highlights
how seismometers not only detect natural events like storms but also everyday
human activity, offering a unique look into the vibrations around us.
Giuseppe
and I will be doing regular check-ups and data downloads from each seismometer
about every 2 to 3 months to keep everything running smoothly. If you happen to
spot us out in the field while we are installing or servicing the instruments
(don’t worry — we always have the landowner's permission), feel free to come
say ‘Hi’ and ask us about the project!
Images: After
a sunny day out in the field, Giuseppe and Colin wrapped up the installations
at two different stations. The setup is looking solid — with the waterproof
black box keeping our batteries and cables safe and dry (Photo: Giuseppe Maggio); Seismic
data from station ANT21 reveals ground movement caused by Storm Éowyn.
DIAS is a GEMINI partner.