1:09 PM – Light Earthquake Recorded Southeast of Guadeloupe

At 1:09 PM Saturday, February 17th, 2024, the University of the West Indies Seismic Research Centre (UWI SRC) recorded a light earthquake of magnitude 4.1 (mt) southeast of Guadeloupe.

The earthquake was preliminarily located at 60.79°W and 15.930°N, approximately 90 kilometers southeast of Point-à-Pitre, Guadeloupe, 96 kilometers northeast of Roseau, Dominica, and 151 kilometers north-northeast of Fort-de-France, Martinique. The event was located at a depth of 10 kilometers.

Information from the UWI SRC concerning the earthquake southeast of Guadeloupe
Information from the UWI SRC concerning the earthquake southeast of Guadeloupe

This information is preliminary from the UWI SRC, the authority for seismic and volcanological information in the English-speaking Eastern Caribbean. Quake parameters may change upon further review by an analyst at the UWI SRC.

There have been no reports of shaking at any of the nearby islands. 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:

  1. The earthquake must occur beneath the ocean or cause material to slide within or into the ocean.
  2. The earthquake must be strong, with at least a magnitude of 6.5.
  3. The earthquake must rupture the Earth’s surface, and it must occur at a shallow depth – less than 70 kilometers below the surface of the Earth.
  4. 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 across the globe. 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.

The Bureau Central et Sismologique Français – Réseau National de Surveillance Sismique, the French national facility dedicated to the monitoring and analysis of French seismic activity, reviewed this event and calculated a magnitude of 3.3, at a depth of 27 kilometers, in a similar location at 15.97°N, 60.79°W.

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Earthquake magnitude is a quantitative, mathematical calculation to measure the energy released at the source of an earthquake. On the other hand, earthquake intensity is the qualitative…

Can earthquakes be predicted or forecasted?

Earthquakes cannot be predicted based on current research and technology. Earthquake prediction is a branch of seismology focused on predicting an exact time, location, and magnitude of an…

Within 20 kilometers of Saturday afternoon’s earthquake, there have been over 800 events recorded in the last 70 years. The largest recorded event within 20 kilometers of Saturday’s quake occurred on August 2nd, 1992, registering a magnitude of 5.6 on the Richter Scale. Seismic events in this area generally occur at depths between 10 to 35 kilometers below the surface, but events as deep as 110 kilometers have been recorded.

Has there been an increase in seismic activity?

Seismicity across Trinidad and Tobago, showing thousands of earthquakes recorded since 1960.
Seismicity across Trinidad and Tobago, showing thousands of earthquakes recorded since 1960.

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 has said regional seismic and volcanic activity has been elevated for several years in its annual report for 2020 to 2021.

On average, the Eastern Caribbean has seen a pattern of major (M7.0-M7.9) quakes every 20 to 30 years. 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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