QuakeShake

QuakeShake

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Quake Shake is a vibrant community of citizen seismologists in Ireland.

QuakeShake: Shaking up earthquake awareness in Ireland ๐Ÿ‡ฎ๐Ÿ‡ช Join our seismic network of citizen seismologists monitoring Irish and global earthquakes ๐Ÿ—บ๏ธ
Find more information at our website below โฌ‡๏ธ The programme is co- funded by Dublin Institute for Advanced Studies (DIAS) and Geological Survey Ireland (GSI). Our mission is to to engage Irish society to contribute to the observation and study of ea

Photos from QuakeShake's post 28/05/2026

A M6.9 earthquake has occurred northern in Northern Chile on 25 May 2026 at 21:52 UTC. The earthquake occurred approximately 29 km east-northeast of Calama in the Antofagasta Region, at a depth of 109 km. The earthquake occurred within one of the most seismically active regions in the world, along the boundary where the Nazca Plate is subducting beneath the South American Plate. This tectonic setting is responsible for many of Chileโ€™s largest and most destructive earthquakes. Intermediate-depth earthquakes such as this one commonly occur within the descending Nazca Plate beneath the Andes Mountains.

According to the United States Geological Survey (USGS), residents in Calama and surrounding communities reported strong shaking, and some temporary power and water interruptions occurred following the event. Chilean authorities also reported minor landslides within the Antofagasta Region. However, there were no immediate reports of fatalities or major structural damage.

Chile experiences frequent earthquakes due to its location along the Pacific Ring of Fire. The country has a long history of major seismic events, including the 1960 Valdivia earthquake โ€” the largest instrumentally recorded earthquake in history at magnitude 9.5.

Photos from QuakeShake's post 01/05/2026

Oh goly gosh last week was busy๐Ÿ˜ƒ Here is a throwback to some of the highlights:

Friday we attended the National Marine Environment Conference organised by and ๐Ÿ‘ ๐ŸŒŠ Our highlight was incredible presentation of the fin whale calls they recorded with their QuakeShake seismometer ๐Ÿ‹ We had our own display stand with an Orca and Raspberry Shake seismometer recording the event๐ŸŽค ใ€ฐ๏ธ .collins.3766

Also on Friday, UCD professor Aline Melo displayed one of our Raspberry Shakes at her daughter's primary school show and tell in Co. Wicklow. One of the students enjoyed irish dancing beside the shake ๐Ÿ‘ฏโ€โ™€๏ธ

Thursday we presented for
Marine Week live webinar about the QuakeShake programme and fin whales ๐Ÿ™‚

Wednesday to Monday we attended the British Seismology Meeting in Leeds Univeristy England and presented a presentation and poster. A highlight was learning alot about other seismology outreach programmes ๐Ÿ‘

Overall a fantastic week and thanks to all the incredible organisers!

Photos from QuakeShake's post 21/04/2026

On the 20th April 2026, at 07:53:00 UTC (17:53:00 local time), a powerful earthquake measuring M7.4 struck at a depth of 35km offshore Honshu, about 100 km ENE from Miyako, see the red circle marking the epicentre in the map in picture 2.The earthquake resulted from thrust faulting in the subduction zone between the Pacific and North America plates. A tsunami was triggered and according to the Japan Meteorological Agency (JMA) about 40 minutes after the earthquake origin time an 80-centimetre wave hit a port in Kuji in Iwate. A tsunami warning was issued for Japanโ€™s coastline, with waves expected to reach up to 3 meters, but the threat did not materialize, and authorities lifted the warning shortly afterward. No damage has been reported so far, but the earthquake was felt in buildings as far away as Tokyo, approximately 400 kilometers from the epicenter.



09/04/2026

You might think when you look at the ๐ŸŒ‘ that its very quiet and inactive geologically speaking..... but moonquakes do occur! Just not how we are used to ๐ŸŒquakes happening.

Unlike here on Earth they aren't mainly caused by active moving tectonic plates. Moonquakes can be triggered by Earth's gravitational pull, the moon cooling and shrinking, meteorite impacts, temperature changes and us.

We know all of this thanks to the Apollo missions ๐Ÿš€๐Ÿ‘จโ€๐Ÿš€

Nunn et all paper available at https://link.springer.com/article/10.1007/s11214-020-00709-3



26/03/2026

We have written a blog for detailing all of our exciting findings using citizen Raspberry Shake seismometers to track fin whales ๐Ÿ‹ ๐Ÿ˜€

You can listen to the actual recordings of a fin whale singing off the coast in Waterford which was recorded by former QuakeShake station RBB07 ๐Ÿ”Š
And read to find out about the Christmas Day surprise ๐Ÿ˜ฎ ๐ŸŽ„๐ŸŽ

We have more fin whale recordings since our public meeting in the Copper Coast Geopark back in June 2025 so thanks to all of our citizen seismologist hosts for attending and hosting our shakes ๐Ÿ‘

Thanks to the Irish Whale and Dolphin Group for their excellent sightings data ๐Ÿณ

๐Ÿ‘‰Read more about the findings at our website: www.quakeshake.ie/2025/12/17/citizen-scientists-track-fin-whales-on-irelands-copper-coast/

๐Ÿ”—Or Raspberry Shakes website: www.raspberryshake.org/citizen-scientists-track-fin-whales-on-irelands-copper-coast/
www.quakeshake.ie/2025/12/17/citizen-scientists-track-fin-whales-on-irelands-copper-coast/

10/03/2026

Apologies for such a long video!๐Ÿ™ˆ I started making this video back in February when a magnitude 7.1 earthquake occured beneath Borneo with a deep epicentre of 620 kilometres. This wasnt well recorded by our Raspberry Shake seismometers as this part of the world is a bit of a longitude and latitude shadow for some Irish seismometers. Then yesterday there was a Magntude 6.0 Italian earthquake that also occurred at a very deep depth (USGS says 373km and INGV say 414km) and this got me thinking again about deep earthquakes and how they occur ๐Ÿค”

Most earthquakes happen near the Earthโ€™s surface (within about 70 km). Sometimes they occur hundreds of kilometers deep. At such depths, rocks are under extreme heat and pressure, so they usually bend instead of breaking, which is why deep earthquakes were once thought impossible. ๐Ÿชจ

They occur in areas of subduction, where one tectonic plate sinks beneath another. A cold, dense oceanic plate sinks into the mantle and remains cooler and more brittle than the surrounding rock. As it descends (sometimes 300โ€“700 km deep), intense pressure can cause sudden cracking or mineral changes, releasing energy as an earthquake ใ€ฐ๏ธ

Because these earthquakes happen deep inside the sinking plate, the shaking at the surface is often weaker than for shallow earthquakes of the same size.



10/03/2026

Apologies for such a long video!๐Ÿ™ˆ I started making this video back in February when a magnitude 7.1 earthquake occured beneath Borneo with a deep epicentre of 620 kilometres. This wasnt well recorded by our Raspberry Shake seismometers as this part of the world is a longitude and latitude shadow for Irish seismometers. Then yesterday there was a Magntude 6.0 earthquake that also occurred at a very deep depth (USGS says 373km and INGV say 414km) and this got me thinking about deep earthquakes and how they occur ๐Ÿค”

Most earthquakes happen near the Earthโ€™s surface (within about 70 km). Sometimes they occur hundreds of kilometers deep.

At such depths, rocks are under extreme heat and pressure, so they usually bend instead of breaking, which is why deep earthquakes were once thought impossible.

They occur in areas of subduction, where one tectonic plate sinks beneath another. A cold, dense oceanic plate sinks into the mantle and remains cooler and more brittle than the surrounding rock. As it descends (sometimes 300โ€“700 km deep), intense pressure can cause sudden cracking or mineral changes, releasing energy as an earthquake ใ€ฐ๏ธ

Because these earthquakes happen deep inside the sinking plate, the shaking at the surface is often weaker than for shallow earthquakes of the same size.


Photos from QuakeShake's post 26/01/2026

Congratulations to students Chloe, Victoria, Veronika and Marylyn who presented projects at the Stripe Young Scientist and Scifest ๐Ÿ‘We are so proud to see them incorporating QuakeShake data ใ€ฐ๏ธ๐Ÿ™Œ

Chloe utilised RSAM data compiled by INSN technical officer James Grannell to compare storm data on Inis Meรกin Island.

Victoria, Veronika and Marylyn used our locate the epicentre of an Irish Earthquake to analyse how earthquakes are located.

We know a huge amount of work goes into putting these projects together so we'll done to students, teachers, family and friends!๐Ÿ˜ƒ

If you would like our assistance with a project for a science fair please feel free to contact us.

Photos from QuakeShake's post 05/12/2025

Did you know Raspberry Shake seismometers from the QuakeShake programme have picked up low-frequency fin whale calls off the Copper Coast in County Waterford? ๐Ÿ‹These land based seismometers designed to record earthquakes are doubling as coastal โ€œears,โ€ capturing the deep vocalisations of fin whales passing close by offshore. ๐ŸŒŠ

Martin first detected these calls by analysing seismic data from a Raspberry Shake located in the Copper Coast Geopark. During our annual meeting this June, we expanded the network by distributing more Raspberry Shakes along the south-east coast, increasing our chances of capturing additional fin whale song, see slide 4.

What the map in slide 4 shows:
โ€ข Yellow triangles โ€” QuakeShake Raspberry Shake stations located in schools (), homes, and the Copper Coast Geopark.
โ€ข Red dots โ€” Confirmed whale sightings provided by the Irish Whale and Dolphin Group (IWDG).๐Ÿณ
โ€ข On the right, spectrograms (yellow) and seismograms (blue) from these stations (band-pass filtered at ~18โ€“23 Hz) reveal the characteristic low-frequency pulses of fin whale song.

These detections reveal that fin whales singing just offshore are powerfull enough for their deep vocalisations to travel through the water, couple into the seafloor, and register as ground vibrations several kilometres inland. Its cool that this singing is all picked up by citizen science seismometers ๐ŸŽถ

To learn more, check out Martinโ€™s โ€œSamhain agus Scienceโ€ presentation:
https://www.youtube.com/watch?v=pkP5oB94Fho&list=PLt_XradIp-myGuKol5CY2e2QTCWGIm_sb&index=6

And read the full research paper here:
https://www.nature.com/articles/s41598-025-97638-4

04/12/2025

On the 3rd of December 2025 at 23:23:34 UTC an earthquake of magnitude M3.2 occurred in Lancashire, northwestern England. The earthquake occurred at a depth of 3 km, and located 14 km north of the city of Lancaster.

Here is the earthquake recorded by Irish

According to the British Geological Survey (BGS), 471 felt reports were received from members of the public, at the time of writing. The overall intensity for this event corresponds to Felt V (strong) of the European Macroseismic Scale (EMS). The map below (produced by the BGS) shows the locations of where the felt reports originated, with felt intensities aggregated into 5km grid squares. More information on this earthquake is available from the BGS website at: https://earthquakes.bgs.ac.uk/earthquakes/recent_events/20251203232333.html =macroseismic

Earthquakes tend to occur much more frequently in Britain than in Ireland, with the rate of seismicity about 10 times higher in Britain than Ireland. In addition, earthquakes with magnitude greater than M3 do occur in Britain, albeit infrequently. One of the most notable British earthquakes occurred on the 19th of July 1984, when a M5.4 struck the Lleyn Peninsula in northwest Wales. This event was widely felt by the public in Britain and Ireland, whereby the INSN received hundreds of felt reports from across Leinster.

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