Earthquake Recorded Northeast of Antigua and Barbuda

At 9:46 PM Wednesday, April 10th, 2024, the University of the West Indies Seismic Research Centre (UWI SRC) recorded a minor earthquake of magnitude 3.7 (mt) north of Antigua.

The earthquake was located 82.2 kilometers northwest of Saint John’s, Antigua and Barbuda, 107.7 kilometers north of Brades, Montserrat, and 75.5 kilometers northeast of Basseterre, Saint Kitts, and Nevis. It was at a depth of 53.1 kilometers.

Information from the UWI SRC concerning the earthquake near Antigua and Barbuda

The UWI SRC, the authority on seismic and volcanological information in the English-speaking Eastern Caribbean, has reviewed this information. There have been no felt reports at this time. 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 occur at a shallow depth—less than 70 kilometers below the surface.
  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 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 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…

Based on historical and instrumental records, 215 events have occurred within 20 kilometers of Wednesday’s earthquake. The largest recorded event within 20 kilometers of Wednesday’s quake occurred on October 16th, 1961, registering a magnitude of 5.7 on the Richter Scale. Seismic events in this area generally occur at depths shallower than 30 kilometers, but events have been recorded as deep as 218 kilometers below the surface.

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’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. 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.

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