Light Earthquake Recorded North-northeast of Tobago

At 10:31 PM Friday 7th May 2021, a (preliminary) light Magnitude 4.3 (MLv) earthquake occurred approximately 121.0 km NW of Bridgetown, Barbados, 122.0 km SE of Kingstown, Saint Vincent and the Grenadines and 140.0 km NNE of Scarborough, Trinidad and Tobago. This event was located at 60.418°W and 12.404°N, at a depth of 59.0 Kilometers.

The above information is preliminary from the U.W.I. Seismic Research Centre, the authority for seismic and volcanological information in the Eastern Caribbean. Parameters may change as more data is received and reviewed by seismologists.

This event was reported felt in Barbados. You can submit felt reports to the University of the West Indies Seismic Research Centre or the United States Geological Survey.

UWI SRC's solution for the light earthquake northeast of Tobago on Friday night.
UWI SRC’s solution for the light earthquake northeast of Tobago on Friday night.

The above information is preliminary from the U.W.I. Seismic Research Centre, the authority for seismic and volcanological information in the Eastern Caribbean. Parameters may change as more data is received and reviewed by seismologists.

Seismic data from a seismometer stationed on Grenada, capturing the M4.4 earthquake at 10:31 PM, seen by the large spike in amplitude at 3:31 (accounting for the delay in seismic waves to travel from the hypocenter to the seismic station) (IRIS)
Seismic data from a seismometer stationed on Grenada, capturing the light earthquake at 10:31 PM, seen by the large spike in amplitude at 3:31 (accounting for the delay in seismic waves to travel from the hypocenter to the seismic station) (IRIS)

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 in the ocean.
  2. The earthquake must be strong, at least magnitude 6.5.
  3. The earthquake must rupture the Earth’s surface and it must occur at shallow depth – less than 70 KM below the surface of the Earth.
  4. The earthquake must cause vertical movement of the seafloor (up to several meters).

These conditions were not met.

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 ranges of the data’s uncertainty. This is generally accepted within the scientific community.

USGS' solution for the light earthquake northeast of Tobago on Friday night.
USGS’ solution for the light earthquake northeast of Tobago on Friday night.

At 10:31 PM Friday 7th May 2021, a (reviewed) light Magnitude 4.4 (mb) earthquake occurred approximately 128.3 KM SSW of Bridgetown, Barbados, 129.6 KM NE of Scarborough, Trinidad and Tobago, and 197 KM SE of Kingstown, St. Vincent and the Grenadines. This event was located at 59.870°W and 11.981°N, at a depth of 10.0 Kilometers. This information has been reviewed by the United States Geological Survey.

Based on the location and depth of this quake, it is tectonic in origin and occurred within the overriding Caribbean Plate. In this area, the South American plate is beginning to descend into the Earth’s mantle. In this location, the subducting slab is at approximately 45 kilometers depth.

Earthquakes *cannot* be predicted – meaning the precise time, date, magnitude, depth, etc. cannot be known ahead of time based on current research and technology.

Earthquakes *cannot* be predicted – meaning the precise time, date, magnitude, depth, etc. cannot be known ahead of time based on current research and technology.

Generally, across the Eastern Caribbean, a seismically active area, earthquakes of this magnitude, up to M8.0 and greater, are possible and this statement has been repeated by seismologists at the U.W.I. Seismic Research Centre for decades.

Each year, over 2,200 seismic events are recorded in the Eastern Caribbean. 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 great quakes (M8.0+) on the Richter Scale have occurred every century or so in the region. The probability of another event at that level is high since the last >M8.0 earthquake occurred in 1843.

Now is the time to create or go over your earthquake preparedness plan and know what to do during, before, and after an earthquake.

Facebook Comments