At 7:09 PM Monday, March 25th, 2024, the University of the West Indies Seismic Research Centre (UWI SRC) recorded a minor earthquake of magnitude 3.7 (mt) northeast of Guadeloupe.
The earthquake was preliminarily located at approximately 10.432 kilometers northeast of Point-à-Pitre, Guadeloupe, 159.04 kilometers east-southeast of Brades, Montserrat, and 127.67 kilometers southeast of Saint John’s, Antigua and Barbuda. The event was located at a depth of 30.8 kilometers.
The UWI SRC, the authority on seismic and volcanological information in the English-speaking Eastern Caribbean, has reviewed this information.
No reports of shaking at any of the nearby islands have been received. However, you can submit felt reports to the University of the West Indies Seismic Research Centre.
There is no tsunami threat.
There are four conditions necessary for an earthquake to cause a tsunami:
- The earthquake must occur beneath the ocean or cause material to slide within or into the ocean.
- The earthquake must be strong, with at least a magnitude of 6.5.
- The earthquake must rupture the Earth’s surface and occur at a shallow depth—less than 70 kilometers below the surface.
- The earthquake must cause vertical movement of the seafloor (up to several meters).
None of these conditions occurred.
Note that different seismic monitoring agencies use different methods, or several methods, for processing quake parameters worldwide. Each method has its limitations and will likely produce different results within the range of the data’s uncertainty. This is generally accepted within the scientific community.
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Earthquake Magnitude & Intensity
Can earthquakes be predicted or forecasted?
Nearly 300 events have been noted within 20 kilometers of Monday night’s earthquake across both instrumental and recorded history. The largest recorded event within 20 kilometers of Monday’s quake occurred on March 26th, 2021, registering a magnitude of 6.0 on the Richter Scale. Seismic events in this area generally occur at depths between 0 and 50 kilometers below the surface, but events as deep as 95 kilometers have been recorded.
Has there been an increase in seismic activity?
Trinidad and Tobago and the surrounding region are very seismically active. Across the Eastern Caribbean, over 2,200 earthquakes are recorded annually. Since 1990, the University of the West Indies Seismic Research Centre has recorded an annual average of 280 earthquakes in the Trinidad and Tobago region (area bounded by 9.5°- 11.5°N & 59.5°W – 63.5°W). Of these 280 quakes, 50 of these seismic events are, on average, above magnitude 3.5.
Most earthquakes occur northwest of Trinidad in an area known as North of the Paria Peninsula, which has the second-highest seismicity in the Eastern Caribbean. According to the UWI SRC, approximately 65 events of magnitude 2.1 and above are located in the area annually.
However, the UWI SRC’s annual report for 2020 to 2021 states that regional seismic and volcanic activity has been elevated for several years.
On average, the Eastern Caribbean has seen a pattern of major (M7.0-M7.9) quakes every 20 to 30 years, and that pattern has stayed true. The last major (M7.0-7.9) quake occurred north of Martinique in 2007.
Historical patterns indicate that great quakes (M8.0+) on the Richter Scale have occurred every century in the region. The probability of another event at that level is high since the last >M8.0 earthquake occurred in 1843. While it is impossible to say definitively when the next great quake will occur in the region, the time since the last one is now more than 170 years ago.
It is important to note seismic activity *cannot* be predicted – meaning the precise time, date, magnitude, depth, etc., cannot be known ahead of time based on current research and technology.
Now is the time to create or go over your earthquake preparedness plan and know what to do during, before, and after an earthquake.
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In our region, earthquakes can strike at any time and any place, so it is important to know how to keep yourself safe when one strikes.
