5.1 Atlantic earthquake rattles; There is no tsunami threat

The strong earthquake occurred near the equator in the Atlantic Ocean. Photo: USGS

A 5.1-magnitude earthquake struck below the central Atlantic moments ago. Fortunately, there is no risk of a tsunami.

The epicenter of the strong earthquake was about 6 miles deep, and located at 0.081 degrees N 17.393 degrees W. The earthquake was far enough off the ground for no one to feel it.

The earthquake occurred in a seismically active region in the mid-Atlantic, separating the South American Plate from the African Plate. In this part of the world, the two plates are moving apart, causing earthquakes as they split over the edge.

These plates are based on the scientific theory of plate tectonics, which describes the large-scale motion of the plates that make up the Earth’s lithosphere. Scientists believe that tectonic processes began on Earth between 3.3 and 3.5 billion years ago, based on the concept of continental drift, a scientific concept developed in the early part of the twentieth century. Continental drift is the gradual movement of continents across the Earth’s surface through geological times.

Tsunamis are giant waves caused by earthquakes or volcanic eruptions under the sea. In the depths of the ocean, tsunamis do not get much higher. But as the waves travel inland, they accumulate at higher and higher altitudes as the depth of the ocean decreases. According to the National Ocean Service, the speed of a tsunami waves depends on the depth of the ocean rather than the distance from the wave’s source. Tsunami waves may travel at the same speed as jets over deep water, slowing down only when they reach shallow waters. While tsunamis are often referred to as tidal waves, this name is discouraged by oceanologists because tides have nothing to do with these gigantic waves.

Today’s earthquake was not far from the 5.0 earthquake that struck the mid-Atlantic on April 4.

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