At 7:28 AM on Tuesday 18th June 2019, a Magnitude 4.7 (Md or mt) earthquake occurred 88 km W of Port of Spain, Trinidad and Tobago and 104 km E of Carúpano, Venezuela. This event occurred at a shallow to an intermediate depth of 53.0 Kilometers. This information (above) is preliminary from the U.W.I. Seismic Research Center and is subject to change upon review by a seismologist at the Seismic Research Center.
This earthquake was widely reported felt with a short jolt across parts of Northwestern, North-Central, Western and Central Trinidad as well as parts of Northeastern Venezuela.
The Venezuelan Foundation for Seismological Research (FUNVISIS) has published its preliminary solution slightly closer to Trinidad at 29.5 km N of Güiria, Venezuela, 85.8 km W of Port of Spain, Trinidad and Tobago and 108.96 km NW of San Fernando, Trinidad and Tobago. FUNVISIS placed this quake at a shallower depth of 27.3 kilometers and a lower magnitude of 4.2 (MW). This information (above) is preliminary from the FUNVISIS and is subject to change upon review by a seismologist at FUNVISIS
Note that across the globe, different seismic monitoring agencies use different methods, or several methods, for processing earthquake parameters. Each method has its limitations and will likely produce different results within the ranges of the uncertainty of that data. This is generally accepted within the scientific community.
This event was not reported felt across Trinidad. You can submit felt reports to the University of the West Indies Seismic Research Centre.
Based on the location of this earthquake, NW of Trinidad, it likely occurred in seismic zone 1. Within zone one, two main mechanisms drive seismic activity.
Firstly, the South American plate is beginning to rapidly descend into the Earth’s mantle as the detached oceanic lithosphere exists at depths between 50 to 300 kilometers. (Russo et al. 1993). This zone is one of the most active seismogenic sources in the Eastern Caribbean and has the potential to generate earthquakes up to Magnitude 8.0. Earthquakes deeper than 50 kilometers are characteristic for this subduction area.
Secondly, at shallower levels, such as where this earthquake occurred according to UWI SRC and FUNVISIS, the North Coast Fault Zone, as well as the El Pilar Fault, part of the Boconó-San Sebastian-El Pilar Fault system, runs across Zone 1. These fault systems compensate for the stress built up as the Caribbean plate slides past the South American plate. Hence, most of these earthquakes from these fault systems are between 0 to 50 kilometers.
This area has some of the highest seismicity in the Eastern Caribbean, and this location accounts for the greatest number of earthquakes in the Trinidad and Tobago region. Strong earthquakes in this area have occurred in the past, with the largest being over magnitude 7.0.
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, in Trinidad and Tobago, a seismically active area, earthquakes of this magnitude, up to M8.0 and greater, are possible in area, 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 earthquakes (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. See here for more details.